Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
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Maria V. Alvanou
Abstract
Biofouling constitutes one of the main obstacles in the sector of shellfish farming. Under this perspective, it is of highly importance to critically combine the updated information regarding the invasive potential of ascidian species, together with the factors contributing toward these events. The biological features of each species in relation to the gathering of the main non-indigenous species in the Mediterranean basin represent the first step toward mitigation of negative effects of the phenomenon. Further, there are limited studies investigating the physiological changes of bivalves caused by biofouling while leading to an increase in stress biomarkers. In the present review, the major ascidian species negatively affecting bivalve culture in the Mediterranean Sea are presented, alongside monitoring of ascidians from four Greek mussel farming locations as typical mussel culture cases. Among the main ascidian species, Styela plicata, Clavelina oblonga, Ciona robusta, Aplidium sp., Didemnum sp., Botryllus schlosseri, and Didemnum drachi are included, with the last three being the most harmful for this aquaculture sector. Based on the existing literature and research conducted so far, future research directions are proposed, in an effort to effectively control or efficiently manage ascidian biofouling organisms. Overall, perspectives toward the way we manage the biofouling phenomenon, such as the use of ascidian’s by-products in feedstuffs, chemical and pharmaceutical industry, or their incorporation in bivalve co-culture and integrated multi-trophic aquaculture systems represent promising alternative approaches.
1 Introduction
Following the continuous growth of the human population, there is an urgent need for sustainable aquaculture development, keeping in mind that it constitutes one of the fastest-growing food production industries [1]. The aquaculture sector represents a commercial activity with a sharp increase during the last years [2]. Aquaculture, apart from seafood production contributes to wild population retention, as it leads to natural catch reduction [3]. Generally, bivalve culture contributes to 60% of the global marine aquaculture production [4]. More specifically, bivalve farming is categorized among the most sustainable aquaculture forms [5]. Within cultured bivalves, oysters, clams, scallops, and mussels are included, with the latter characterized by a total yield of 2 million tons per year, equal to 94% of the total harvest, demonstrating the major role that farming enacts in mussel production [6]. Marine bivalves are rich in proteins and are characterized as high-value aquatic products oriented for human consumption [7]. Bivalve populations, both from natural and cultured stocks, suffer from severe losses due to several pathogens [8,9], biofouling [10], heat waves [11], and urban and agricultural wastes [12].
Among the main threats bivalve aquaculture faces, the biofouling phenomenon refers to the accumulation of undesirable organisms on the underwater surfaces [10]. Biofouling threatens the marine aquaculture industry both from a profitability and a viability point of view, as it is responsible for periodic mortality and removal of fouled organisms [13]. Additionally, biofoulants cause severe negative outcomes on yield and growth rates of cultured species [14,15]. Economic losses owing to biofouling are calculated at the levels of 5–10% of the total production value [16]. Further, regarding the market price, the above phenomenon may cause 20 and 30% losses for oysters [17] and scallops [18], respectively. Nevertheless, it needs to be mentioned that losses due to biofouling can significantly fluctuate between aquaculture locations and cultured species, mainly associated with the different practices that farmers use in each condition [19].
Apart from the economic losses, biofouling is also responsible for ecological disturbances with biofoulant organisms characterized by high spread rates and frequent population outbreaks [20]. Considering bivalve aquaculture species, both bivalve shells and artificial substrates provide ideal extended submerged surfaces [21], free of predators, constructing a safe place for fouling organisms to grow [22]. Additionally, fouling organisms are characterized by high invasive potential, increased tolerance, and easy adaptation to new ecosystems. All of these can transform them into the dominant organisms of the new habitat [23]. Furthermore, plenty of biofouling species are competitive toward space and can succeed high biomass and densities in short time periods [24].
One of the most harmful and prolific biofouling communities toward shellfish aquaculture is the ascidian species [25] which grow as independent individuals and occasionally establish aggregations mainly due to their high fecundity [26]. Further, apart from the aggregation they also include colonial forms. Ascidians (Phylum: Chordata, Sub-phylum: Tunicata) also known as “sea squirts” colonize a plethora of surfaces located underwater and, although their dispersal capacity is low, human activities such as trade via shipping can result in their increased geographic spread [27,28]. Keeping in mind that their geographic expansion is enhanced by human actions, their high invasion ability is accompanied and attributed to many factors including their ability to regenerate from fragments, their short period for reaching sexual maturity, their high growth rate, hermaphroditism, high fecundity, dispersal of pelagic larval phase, their ability to produce metabolites that are often harmful to predators, and extended reproduction period [29,30].
Knowledge regarding the invasive ability of the main ascidian species in the Mediterranean Sea toward bivalve aquaculture, their presence in bivalve farms, as well as the physiological impact of biofouling phenomenon on the fouled organisms is of high importance for the design of effective mitigation strategies. Thus, the scope of the present review can be summarized in four basic components: first, to collect the main factors contributing to ascidian dispersal and their invasion success; second, to gather the main non-indigenous species (NIS) in the Mediterranean region; third, to critically discuss the above topics with the combination of novel data concerning the presence of ascidian species in a typical paradigm of bivalve aquaculture negatively influenced by the presence of those biofoulants, i.e. long line mussel farming from Greece; and lastly, to highlight the research gap concerning the physiological impact of fouling on farmed animals. Keeping in mind that the problem of ascidians still exists, our scope was additionally to propose the future research aims that have to be targeted to mitigate the negative impacts of biofouling in bivalve aquaculture.
2 Ascidians’ dispersal and invasion capability
Estimation of the dispersal potential of invasive species is of high importance in an effort to design appropriate management practices [31]. More specifically, to succeed in an in-depth understanding of the invasion potential of invasive species in the field, some of the major fundamental steps concern the investigation of dispersal vectors and distances, propagule supply, interactions between species, diversity of resident communities, disturbance regimes, environmental conditions encountered, and predator–prey relationships [32].
A key feature in the life cycle of benthic marine invertebrates is the limited adult movement, which influences the dispersal of pelagic early life stages [33]. The dispersal of the planktonic propagule, which is a major parameter toward the connection of geographically separated marine populations, together with the spread and the persistence of native populations, lead to the re-establishment in previously introduced areas and the definition of species’ range limits [34]. The dispersal capability is influenced by many factors including food resources, pelagic larvae duration, behavior (migration type), predators, and oceanographic conditions such as sea currents [35]. Factors related to human activities, e.g., the influence of the global trade by ascidian growth on the keels of boats and ships, contribute to a great extent in the further geographic spread even at a global scale, as they accelerate the spread rates by carrying them within ballast water; attached to vessel hulls [36,37], aquaculture [38], and recreational and fisheries watercraft [39].
Ascidians have generally aroused interest on account of their high invasive nature, i.e., due to propagule pressure; release of enemies and environmental changes, and their potential environmental impacts [20,40]. They are sessile filter-feeders, categorized among the main biofouling taxa with several cosmopolitan species successfully established worldwide [41,42]. Ascidian species can adapt in a wide range of salinities, temperatures [43], and highly polluted areas [44], whereas they can flourish when the organic load is enriched [36]. Ascidians do not have a long dispersal larva, but they are characterized by a short-lived tadpole larva that usually disperses just several meters or even less, especially regarding colonial species [45]. There are some exceptions where larvae live for many days and move with the aid of currents, e.g., 1–5 days for Ciona intestinalis and rafting of fragmented colony parts in colonial species (e.g., Botrylloides violaceus) that can contribute to wider natural dispersal [46,47]. Further, it has been reported that ascidian species can spread as they attach to other species such as American lobsters (Homarus americanus) and rock crabs (Cancer irroratus) [38]. Thus, human-mediated introductions have been recorded in all continents except Antarctica [20]. On the other hand, invasive species originating from Antarctica have invaded southern regions [48].
Hence, there are plenty of vectors contributing to the transport of the non-indigenous ascidian (NIA) species into new habitats helping them overcome the geographical barriers and thus spread in new environments. However, the multiple dispersal means and ways do not entail their invasion success. Consequently, ascidian species constitute representative examples of evaluating to which extent dispersal dynamics and geographical distributions contribute to their establishment and domination in new ecosystems.
Apart from understanding the dispersal potential of NIA species, evaluation of the biotic and abiotic factors that lead to the successful establishment of NIA in natural ecosystems constitutes an essential component for mitigating the negative impacts of ascidians’ invasion. As mentioned above, ascidians are tolerant toward a broad range of salinities and temperatures, ranging between 25 and 40‰, and 5–25°C respectively, with some exceptions surviving in even broader ranges including salinities <11‰ and temperatures reaching from −1 to 35°C [20]. Apart from that, ascidians revealed tolerance toward pollution, including heavy metals such as copper, iron, and mercury [49].
Invasive ascidian species usually establish on artificial substrates of harbors and marinas, while there are some cases that later spill over to natural environments as well [50]. It is observed that ascidian species reveal preferences for artificial substrates [51], and therefore, the factors leading to the successful establishment in natural environments have been explored in an effort to explore their spread [52]. In respect to artificial substrates, key factors regarding successful invasion seem to be the absence of predators or failure to recognize introduced prey, diversity of native species, different pollutants, environmental conditions, and propagule pressure [53,54,55,56]; but is this the case for the dispersal in natural substrates as well? It was observed that extended sewage-spill events revealed a decrease in native ascidian species while no significant effect had the proximity to international ports [52]. However, this could be achieved by an indirect pathway as it was observed that the proximity of aquaculture to ports is important for propagule pressure [57]. Temperature has been proposed to be the most important driver for areas suitable for invasion [58] and eutrophication has already been connected with ascidians bio-invasion [36]. Seasonal data described in the present study are in agreement with this fact (see Section 3). Furthermore, when native and invasive populations of the same ascidian species (Herdmania momus) were compared, higher resilience toward higher temperature range was observed in its new habitat in the invasive population. The above observation indicates the important effect of temperature on the invasive ascidians [59]. It has also been observed that the non-native ascidian Ascidia sydneiensis and Phallusia nigra populations had higher tolerance toward a large range of salinities and temperatures in comparison to native species [60]. In a previous study, conducted in regions with colder temperatures, it was observed that invasive ascidians fully colonize underwater surfaces and can thrive in the absence of benthic predators, while this is not the case when the structures are fixed with other benthic organisms [61,62,63].
Apart from the factors contributing to the successful invasion and wide dispersal capacity of ascidian species, it is of main importance to assemble the information regarding the main NIS among the Mediterranean basin to apply a more focused approach toward mitigating the negative effects of the biofouling phenomenon.
3 Major NIA species in the Mediterranean Sea
Apart from the ecological losses, invasive ascidian species possess a serious threat to bivalve aquaculture, marine infrastructures, and fisheries at a global scale through the fouling phenomenon [64]. Many NIA species are considered invasive and constitute a growing global concern [65], with their dispersal enhanced by passive transportation. While biofouling decreases profitability and increases management costs [14], it simultaneously operates as a stepping-stone for the subsequent spread of non-indigenous invasive species along the nearest coastal areas [66].
The Mediterranean Sea is globally considered to be the most invaded sea by NIS [67] and it is recognized as a “hot spot” of biological incursion [64,68]. Plenty of the NIS are transferred into the new environment accidentally by ballast water and tanks, mariculture production [69], ship hitchhikers [70], and through canals [71]. In Greece, there are at least 18 ports with very dynamic operations. Most of the coastal cities in Greece have at least one port receiving cargo and cruise ships [72]. Global regulations aimed to control marine bio-invasions by forcing international ships to manage their ballast water and sediments [73]. More specifically, The International Convention for the Control and Management of Ballast Water and Sediments of Ships was adopted by the International Maritime Organization (IMO), in 2004. To the best of our knowledge, however, there are no regulations concerning the control of ship ballast waters for the presence of invasive species when entering ports, in none of the Mediterranean countries.
Invasive ascidians Ciona sp. and Styela plicata have been introduced in the Mediterranean Sea and are categorized among the most serious ascidian threats. More specifically, S. plicata was first detected in the Mediterranean during the 19th century [74]. Since then, it has been reported in many locations in the Mediterranean Sea such as Israel [75], Italian coasts [76], Aegean and eastern Adriatic Sea [77], and Iberian Peninsula [78]. It is considered a real pest [79] with an impressive ability to survive in many environmental conditions, such as tolerance to moderately wide changes in salinity and temperature [80,81] and high tolerance to water pollution [44]. C. intestinalis was the object of many developmental and evolutionary studies [82]. However, its taxonomic position remains unclear, with at least four cryptic but genetically distinct species. More specifically, C. intestinalis sp. A (assigned to Ciona robusta [83]) is widely distributed in the Mediterranean while sp. B is connected with the “true” intestinalis having a restricted distribution in the Mediterranean. C. intestinalis sp. C has not received a formal name yet, and it was detected in only one place of the Mediterranean Sea [84,85].
Didemnum vexillum is referred to have a negative impact on local biodiversity by rapidly overgrowing on both natural and artificial substrates [47]. It is a very harmful species present in Western Mediterranean [86] and Eastern Mediterranean [87] and is characterized by high dispersal potential, invasiveness, and capability of altering benthic communities [88]. A putative new taxon was detected in Roscoff, France, with the preliminary results supporting the existence of a new species Didemnum pseudovexillum sp. nov with doubts arising regarding the reports of D. vexillum. Although the new species D. pseudovexillum sp. nov is characterized as cryptogenic, there is evidence supporting its introduction [89].
Microcosmus squamiger (Michaelsen, 1927) and Microcosmus exasperatus (Heller 1878) are categorized among solitary ascidian species with their origin probably located in Australia. M. squamiger is invasive in many marine areas globally and has been detected in the Mediterranean Sea since 1995 [44]. After the first detection in Spain, it was also identified in Italy [90]. M. squamiger can form dense, monospecific crusts that outcompete native species in shallow water communities, operating as a threat to Mediterranean littoral communities [91]. M. exasperates has been detected in several locations in the Mediterranean since the 1960s [92] with the most recent one being in Cyprus [93].
The solitary ascidian species H. momus has its native range in Indo-Pacific area and it is supported to have been introduced in the Mediterranean Sea via Suez Canal [94]. Although it was first reported in Egypt, later its presence was demonstrated in Israel, Lebanon [95], Cyprus [96], Turkey [97], and Greece [64], while more recently, it was detected in the central Mediterranean area as well [98]. More importantly, it was observed that the invasive individuals had increased resistance toward higher temperatures in the habitat where they were introduced, implying the ability of the species to further expand its distribution into the Mediterranean [59].
Clavelina oblonga was first and recently recorded in the Mediterranean [99]. However, there is evidence that C. oblonga and Clavelina phlegraea may be the same species, with its presence in Mediterranean known for over 80 years. A bloom of this species occurred late in the summer of 2011 in Spain causing the loss of almost all mussel juveniles [99]. Thus, a lot of attention must be paid, as C. oblonga detected on farmed mussels constitutes a serious stress factor responsible for low productivity and even mortality [100].
The colonial ascidian Botryllus schlosseri is categorized among the most aggressive invaders [101], and it is considered a cryptic species, although some research groups have accepted it as native or introduced [102]. There are five genetically divergent clades (A–E) with clade E identified only in European waters so far [103], while the Mediterranean Sea is proposed to be a center of diversity for this species [104]. It has been recorded in the Mediterranean since the 18th century and in some locations, this species represents a very serious problem for shellfish aquaculture [14]. This species has also established populations in the Eastern Mediterranean since the 20th century [68]. Further, in the Mediterranean, another five Botrylloides NIS have been reported. These species are the introduced B. violaceus, B. pizoni which is a synonym with the invasive B. giganteus [105,106], the Lessepsian migrants B. niger (Herdmann, 1886) and B. anceps (Herdmann, 1891), and B. israelience, the taxonomic status of which remains uncertain [107].
Polyclinum constellatum is a colonial ascidian recently introduced in the Eastern Mediterranean Sea with the first record reported from Egypt in 2016 [108] and a recent record in Greece [109].
Although their presence is not detected so far, two (A. sydneiensis and Didemnum perlucidum) and two (C. intestinalis and Corella eumyota) ascidian species are indicated to have high and intermediate risks, respectively, of introduction and establishment in coastal regions of Mediterranean Sea [101] while A. sydneiensis has been reported as “low risk of introduction” in a recent study [110].
Taking into consideration all the above information regarding the NIS existing in the Mediterranean Sea, a more precise approach to the development of managemental practices will be possible, combining also the data concerning their characteristic toward their dispersal and invasive capability. It should be also mentioned that, although numerous ascidians are considered invasive species, their area of origin is not clarified.
4 Ascidian presence in a typical paradigm of bivalve aquaculture, Greek mussel farming
The shellfish farming sector is of high importance to the Greek national economy supporting regional development, and representing the second most important aquaculture sector after fish farming [111]. Greek seas are very susceptible to invasion of NIS operating as a crossroad between the Black and Red Seas and the Western Mediterranean, enhanced by the high levels of maritime traffic and the presence of several human activities. The Aegean Sea circulation is important and has supported bivalve farming development, mainly by seawater purification [112]. The only cultivated bivalve species in the Mediterranean Sea is the mussel Mytilus galloprovincialis which is farmed mainly in the coastal regions of Northern Greece. Other bivalve species that have been licensed to be farmed in Greece are Ostrea edulis, Ruditapes decussatus, Aequipecten opercularis, and Venus verrucosa [11].
One of the major threats to the bivalve industry is the introduced ascidian species and the biofouling phenomenon that they cause which leads to economic losses [14]. Aquaculture facilities serve as an ideal place for ascidians, as they provide many substrates for attachment, such as ropes, bivalve shells, buoys, and plenty of suspended food. The limited studies with prediction models [101,112] indicate that the main five species with high introduction risk have already been detected in aquaculture facilities [22]. Some of the more aggressive invaders are A. sydneiensis, B. violaceus, B. schlosseri, C. robusta, and D. perlucidum [100]. The most widely distributed species were B. schlosseri and S. plicata. The Mediterranean Sea was characterized by the greatest species richness while it was also included in the regions with the highest risk of primary introductions [101,112].
The ascidian species observed in marine areas characterized by high mussel farming activity in Greece (Figure 1) are shown in Table 1. Generally, an intensively seasonal pattern is indicated, probably influenced by climatic conditions. In Greece, i.e., a typical Mediterranean country of temperate latitude in terms of climatic conditions, summer months are characterized by increased water temperatures, while they are accompanied by heat waves leading to mass mortality events of M. galloprovincialis [113]. Heat waves are expected to be more common during the next years mainly in response to the ongoing temperature increase due to climate crisis. Concerning spring and autumn periods, increased rainfalls have been recorded, while winter periods are generally characterized by colder temperatures. The ascidian species S. plicata is the most common species, whereas C. oblonga, Aplidium sp., Ciona robusta, and Didemnum sp. are present in all marine areas during certain periods. B. schlosseri is characterized by a lower spread, present in Rodopi and Amvrakikos gulf, while D. drachi is detected in three out of four marine areas, namely in Chalastra, Rodopi, and Amvrakikos gulf.

Marine areas in Greece characterized by high levels of mussel farming activity, where high seasonal densities of ascidian presence are observed.
The ascidian species observed in the four sampling sites
Ascidian species | Sampling site | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Rodopi | Chalastra | Amvrakikos | Sagiada | ||||||||||
Date | |||||||||||||
2020 | 2021 | ||||||||||||
25 November | 12 March | 28 April | 18 June | 01 September | 18 November | 26 February | 26 May | 28 June | 30 November | 20 March | 10 September | 01 September | |
Clavelina oblonga | + | + | + | + | + | + | + | + | + | + | |||
Styela plicata | + | + | + | + | + | + | + | + | + | + | + | + | + |
Aplidium sp. | + | + | + | + | + | + | |||||||
Botryllus schlosseri | + | + | |||||||||||
Ciona robusta | + | + | + | + | + | + | + | + | + | + | + | ||
Didemnum drachi | + | + | + | + | |||||||||
Didemnum sp. | + | + | + | + | + | + | + |
An update list of NIS in Greece was conducted by Zenetos et al. [68], including ascidians. More specifically, Ascidiella aspersa, C. robusta, Diplosoma listerianum, S. plicata, and the cryptogenic species B. schlosseri and Clavelina lepadiformis have established populations as they have been found in Greek waters since the 20th century [67]. More recent records of P. nigra and H. momus were made on natural and artificial substrates of Rhodes, Chalkidiki, and Porto Heli Bay for the first one, and in Kastellorizo for the second [63,114,115,116]. Further, Symplegma brakenhielmi was also detected [69] while the colonial ascidian P. constellatum was found in the two westernmost locations of its distribution range, and one of them was the Greek marina in Heraklion [108]. The rare ascidian species Ecteinascidia turbinata was detected along the coasts of Crete Island in 2019 [117]. Even more recently C. oblonga, C. robusta, Botryllus sp., and S. plicata were found to be the dominant biofouling species on farmed mussels in Vistonikos Bay [99].
As the bivalve industry is a well-developed sector in Greece, contributing significantly to the national economy, highlighting the major NIS ascidian species already existing, and causing significant losses in the bivalve farms represent the first step toward their confrontation and management. At the same time, the ones that are present in Mediterranean but not detected in Greece yet can operate as an early sign to be prepared for their possible future dispersion.
5 Physiological impact of ascidians and the fouling phenomenon on farmed bivalves
In the plethora of studies discussing the impact of biofouling on farmed organisms (mainly shellfish), the fitness reduction is claimed as a major impact. Nevertheless, there are some studies reporting that ascidians can also have a positive effect when examined in an ecosystem approach, supporting biodiversity and balance among various taxa [118]. The reduced fitness can be translated by weight, growth, welfare, and survival reduction [119,120,121]. It is proposed that the above parameters are strongly associated with the competition for resources or indirectly via smothering or impede proper valve functioning [122,123,124,125], with, however, limited evidence supporting those observations [20,126]. The majority of the conclusions are drawn from observational studies in which some initial parameters among fouled and non-fouled individuals can lead to confusing results. One representative example that can result in an erroneous assumption is that fouling reduces growth rate when slower-growing stock may present higher susceptibility toward settlement of fouling on shells [20].
A solution to the aforementioned misleading conclusions may be the investigation of the cellular physiology of fouled shellfish. Scarce data existed until recently regarding the effect of biofouling on farmed bivalves. Thus, further investigation of biochemical and physiological indexes estimating the overall well-being of an animal will shed light toward the impact caused by ascidian species on the physiology of cultured fouled and non-fouled bivalves.
In this context, two recent studies from our group investigating the role of temperature fluctuations in comparison with the stress caused by ascidians on the antioxidant defense system, the apoptotic and autophagic pathways, and other physiological stress biomarkers of M. galloprovincialis enlightened the physiological pathways triggering stress attributed to ascidians presence [99,127]. The majority of the biomarkers examined in these two studies revealed elevated levels of stress in fouled mussels compared to non-fouled. Taking into consideration the fact that ascidians cause hypoxia to fouled mussels and that hypoxic conditions favor the increase of reactive oxygen species (ROS) by multiple cellular systems, increased oxidative stress could be the factor triggering both the hsp mRNA levels and the Hsps induction levels in fouled mussels compared to control mussels [99]. The oxidative stress fouled mussels are subjected to, which was evident in these studies both by the downregulated levels of hydroxy-Hif-1α and the increased levels of lipid peroxidation in combination with the enzymatic antioxidant defense system [127]. At the same time, these hypoxic conditions are responsible for the MAPKs’ increased phosphorylation, since it is well-documented that oxidative stress plays a key role in MAPK activation [99]. Since it has been shown that Hsps are induced via MAPK signaling pathways [128,129,130,131], we propose that hypoxia in the fouled mussels first triggers the MAPKs signaling cascade, by phosphorylation, which in turn activates Hsp cytoprotection.
Hypoxic conditions cause oxidative stress leading to cell death pathways activation of the fouled organisms. Specifically, these results indicate that ascidian fouling drives the observed differences in cell death, rather than the temperature. The level of fouling or the species of ascidians covering the mussels may be the leading factor. Moreover, these hypoxia-sensitive organisms exhibited activation of autophagic processes in order for an energy supply to be provided during prolonged hypoxia [126]. The latter goes hand in hand with the fact that epibiotic pressure due to ascidian fauna also triggered the metabolic machinery in order for fouled mussels to exploit all available energy deposits [99]. It is likely that valve closure due to ascidian fouling restricts both feeding and oxygen access. Starvation ignites a metabolic turnover since it affects the utilization of internal energy reserves [132,133,134,135] such as the liver glycogen, which is primarily mobilized for homeostasis of glucose in plasma [136]. It has been shown that food restriction also results in oxidative stress generation in mammals [137,138,139] and fish [140,141]. Probably, the energy reserves’ oxidation through the aerobic pathways can trigger the generation of ROS [142], which can have multifaceted effects on animal physiology. However, we cannot be sure regarding the extent to which each of these parameters (food restriction and oxygen unavailability) contributes, or their synergistic role in the induction of autophagy and the cell death pathway of apoptosis. It should also be noted that the pattern of hydroxy-Hif-1α levels presented herein is similar to the one of apoptosis. This can be attributed to the fact that Hif-1-dependent signaling may play a significant role during hypoxia-induced cell death (Figure 2).

A model of the cellular responses elicited by the effect of ascidian biofouling on Mytilus galloprovincialis.
This enhanced physiological stress seems to be season independent and can be attributed to the oxidative stress and/or feed deprivation caused by ascidian biofouling, thus illuminating the biological impact of this phenomenon. Hence, these two studies provide some clear evidence that ascidian species constitute an important stressor parameter for cultured bivalves.
The gap in the information regarding the physiological mechanisms by which fouling organisms exhibit an adverse impact on farmed animals is eventually emphasized, with only a few conducted studies so far investigating the topic.
6 Discussion
In shellfish aquaculture, ascidian species represent a severe obstacle to bivalve productivity, as they compete with the farmed species for food resources adding weight to the infrastructure, leading to a smaller final size and a higher mortality percentage [143]. Knowledge regarding the presence and biological cycles of the fouling ascidian species is very important for their successful management, and even more important in cases where the seasonality of the fouling species synchronizes with the seasonality of the farmed species [144], while an increase in seawater temperature can contribute to organisms’ invasions [145] which is often the case in bivalve farming.
We can highlight that enlightening the knowledge concerning the dispersal potential of ascidian species is of main importance and necessary for the design of appropriate management practices. For instance, apart from the already known non-indigenous species that negatively impact Greek farmed bivalves, there are records of NIAs species from Turkish and Italian coasts, as well as from other marine areas within the Mediterranean Sea. Thus, probably, it is a matter of time to spread into neighboring waters as well. By understanding the key factors behind their invasion, appropriate measurements can be implemented. Many of the main NIA species have also been observed in Greek locations; however, some of them remained undetected. Additionally, a lot of attention should be paid to ascidian species that are predicted to spread into the Mediterranean Sea, with some of them being characterized by high risk of introduction and establishment (i.e., A. sydneiensis, B. violaceus, and D. perlucidum).
Apart from the observational impacts of the ascidian species on shellfish aquaculture, i.e., increased weight on the ropes of the long line system or the nets and physical damage [18,146], there is evidence that they cause a decrease in the overall shellfish fitness [99,127]. Until recently, apart from limited information [121], scarce data were available regarding the impact of fouling species on fouled organisms on molecular and cellular levels. Recently, it has been observed that in fouled organisms, cell death is more likely triggered by biofouling-related stress rather than from abiotic stress, such as temperature increase [127], and that ascidian biofouling causes starvation stress, therefore triggering several cell protective and signaling pathways in fouled mussels [99].
Although the molecular and cellular mechanisms of the fouled organisms underlying the biofouling phenomenon are still under investigation, the abiotic parameters with special regard to environmental conditions cannot be overlooked. Climate change can operate as a threat toward shellfish production as it may favor ascidian invasions or their increased densities. More specifically, temperature is among the most important abiotic parameters affecting the distribution of the world’s biota [147], while an increase in seawater temperature can contribute to organisms’ invasions [148]. As observed from H. momus populations, invasive individuals had developed resistance toward higher temperatures in comparison with the native ones [58]. Investigation of epigenetic variations can shed some light on the mechanisms underlying the above adaptations to the introduced environment [149]. More specifically, DNA methylation variations were correlated with environmental factors such as temperature and salinity in the highly invasive ascidian species, C. robusta and D. vexillum, implying that these changes can be involved in rapid local adaptations [150,151].
As the impact of climate change on the invasion of ascidian species is well recognized, management strategies are of high importance not only for the protection of biodiversity but for the protection of the bivalve farming sector as well [151]. More specifically, the temperature increase that is expected during the next decades is predicted to cause dramatic changes in both ecosystem structure and function at a global scale. The climate crisis can alter the composition of the biota resident in a specific region by enhancing the spread of invasive species. The temperature increase has a strong influence on ascidian dispersion potential [43,48]. More specifically, following the temperature increase, many ascidian species have expanded their distribution range in regions where they were too cold for their successful establishment [57]. Furthermore, their increased metabolic and reproductive rate according to increased temperature can lead to higher population densities [127]. The alterations in the habitat structure can also contribute to ascidians by eliminating predators or by altering sea currents. There are plenty of treatment methods that have been tested in the past. These methods include organic acids and bases application [152], pressure washing [153], washing with freshwater [154], addition of a culture medium [155], application of silicone release coatings [156], air exposure [157], manual removal of ascidians [158], heat exposure [159], and biocontrol [160]. However, the combination of more than one treatment method is probably more effective while the treatment timing was found to play a crucial role toward successful treatment [153,159]. More attention should be paid toward treatment practices, as in some cases the beneficial impact on farm productivity or farmed organism’s fitness can be more detrimental to cultured shellfish than biofouling removing [126]. Further, apart from the natural compounds that can be used as antifoulants [161], selective breeding can lead to genetic improvement of broodstock which can be resistant toward biofouling [162], whereas simple eco-friendly methods such as aeration and pressure are still applied with high efficiency [163].
One very promising sector rising is the use of ascidian substances to improve human life quality. A number of studies highlight the useful properties of ascidian bioactive compounds [28,164]. Furthermore, toxins produced from ascidian species have been found to exhibit potential toward drug development [165]. Additionally, several ascidian-derived metabolites exhibit antimicrobial properties [166]. Consequently, apart from being a major threat to the shellfish farming sector, bio-invasive ascidian species can operate as a source of high-added value products due to their previously mentioned properties [167].
7 Conclusions and future research directions
The present study follows the above main pathways to reach some conclusions and to summarize some substantial information: first of all, the determination of the main factors contributing to the successful dispersal and invasion of fouling organisms is of critical importance. Second, the gathering of the main NIS in the Mediterranean Sea in combination with the existing knowledge of biological characteristics is the first step toward the development of proper managemental practices. Finally, the investigation of the physiological factors by which fouling organisms cause stress on farmed animals can pause specific targets for mitigating the phenomenon.
In conclusion, biofouling constitutes a serious problem for shellfish aquaculture. There is evidence that ascidians cause stress in fouled organisms at many different levels of biological organization, from the molecular and cellular levels to the organismal and population ones. In the biofouling equation, an important variable is the environmental conditions, which cause additional stress to the cultured organisms. Further, in line with climate change, the invasive ascidian species introduced in bivalve farming areas are increasing. To eradicate the problem, suitable management practices should be implemented, taking into consideration the impact of these practices on cultured bivalves and the balance toward the substantial cost of fouling removal. A rising sector with promising results is the use of bio-invasive ascidians as a source of added value to farmed products due to its bioactive compounds and metabolites that have antimicrobial and antitumoral properties under the scope of drug development (Figure 3).

Schematic depiction of the overall stress of ascidian biofouling on Mytilus galloprovincialis in combination with the main NIS in Mediterranean and some future perspectives that will provide solutions to management efforts.
Despite the plethora of research conducted so far concerning aspects such as species distribution, management strategies, and economic effects on cultured organisms, particular future research goals may provide new perspectives and alternatives in the proper management and control of ascidian biofouling organisms. Based on the aspects analyzed in the present study, we therefore determined and proposed five specific future research goals for biofouling attributed to ascidians.
Although the role of shipping and human transportation in the spread of NIA species is well documented, evaluation of the precise biotic and abiotic factors that lead to the successful establishment of non-indigenous species is crucial. These factors should be emphasized in the different geographic locations taking into consideration the specific oceanographic features of each marine area. Further, ascidian species represent an example of which, although extensive knowledge exists, mainly regarding its ecology, adhesion capability, and surface selection, limited information has been implied toward the development of antifouling surfaces [167].
Ascidian species have been indicated as potential carriers of beneficial food and pharmaceutical ingredients. Thus, in light of the “omics” era, future research should investigate qualitatively and quantitatively the major metabolites that are present in the different ascidian taxa. More specifically, many natural products have been isolated from ascidian species, among the most important being cellulose, which can be found almost exclusively in the ascidian’s tunic. Regarding fatty acids, ascidians can be a good source of n-3 polyunsaturated fatty acids, such as EPA and DHA. Additionally, the inner body is protein rich, which amino-acid composition linked to egg albumin. Further, many other compounds with antifungal, antibacterial, anti-inflammatory, and antitumoral properties such as cyclic peptides, alkaloids, polypeptides, sulfated polysaccharides collagens, sterols, and glycosaminoglycans can be used as by-products. The above-proposed ascidian substances as a good alternative in aquafeeds formulation and in applications in fishing bait, health supplement tablets, as well as in the pharmaceutical and chemical industry [168].
Based on the above, polyculture systems with the simultaneous rearing of low-value bivalves and ascidian for production may be a promising perspective that should be targeted in future studies [169]. Particularly, bivalves that are either of lower economic value or characterized by very large populations may serve as the basis for rearing beneficial ascidians. Apart from that, assuming that in some cases, fouling cannot be avoided due to increased cost, the synchronization of husbandry practices along with fouling patterns may be a possible solution [121,126]. Further, an integrated multi-trophic aquaculture system consisting of the ascidian Styela clava and the sea cucumber Apostichopus japonicus with microalgae was developed to mutually benefit both organisms [170].
So far, research has concluded to the fact that biofouling is responsible for the low productivity of bivalve farms. On the contrary, as described in Section 4, low-productivity mussels may attract more ascidians. Hence, keeping in mind that ascidians foul only partially the mussel lines, ascidian species on mussel farms may serve as the means for selection of higher welfare and fitness mussels, which may perform better against various factors such as seawater temperature and oxygen availability.
Finally, since our knowledge concerning the precise pathways of the physiological stress caused by ascidians on bivalves is only based on very few recent studies, further research should be conducted, utilizing novel technologies such as transcriptomics and epigenetics toward the estimation of the bivalves’ response against biofouling, in both lad and field conditions.
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Funding information: The present work is a part of the project “Development of the best control practices of invasive ascidians in mussel farming infrastructures and remediation of economic effects of invasion” (Code MIS: 5048463) funded by the EU-Greece Operational Program of Fisheries, EPAL 2014–2020.
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Author contributions: M.V.A., K.F., and I.A.G. wrote the draft. I.A.G. and K.F. conceptualized the study. I.A.G. and M.V.A. designed the study. M.V.A. and K.F. visualized the information with figures and graphical abstract. A.T. and D.K.P. collected the data. J.A.T. developed the methodology of the study. M.V.A., K.F., and I.A.G. critically reviewed the study. I.A.G. and K.F. supervised the study.
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Conflict of interest: The authors declare no competing interests.
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- Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
- Research progress of freeze–thaw rock using bibliometric analysis
- Mixed irrigation affects the composition and diversity of the soil bacterial community
- Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
- Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
- Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
- Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
- Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
- Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
- Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
- A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
- Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
- Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
- Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
- Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
- Structural features and tectonic activity of the Weihe Fault, central China
- Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
- Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
- Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
- Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
- Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
- Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
- Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
- Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
- Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
- Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
- Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
- Prediction of formation fracture pressure based on reinforcement learning and XGBoost
- Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
- Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
- Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
- Productive conservation at the landslide prone area under the threat of rapid land cover changes
- Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
- Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
- Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
- Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
- Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
- Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
- Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
- Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
- Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
- Disparities in the geospatial allocation of public facilities from the perspective of living circles
- Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
- Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
- Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
- Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
- Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
- The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
- The critical role of c and φ in ensuring stability: A study on rockfill dams
- Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
- Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
- Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
- Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
- A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
- Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
- Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
- Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
- Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
- Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience
Articles in the same Issue
- Regular Articles
- Theoretical magnetotelluric response of stratiform earth consisting of alternative homogeneous and transitional layers
- The research of common drought indexes for the application to the drought monitoring in the region of Jin Sha river
- Evolutionary game analysis of government, businesses, and consumers in high-standard farmland low-carbon construction
- On the use of low-frequency passive seismic as a direct hydrocarbon indicator: A case study at Banyubang oil field, Indonesia
- Water transportation planning in connection with extreme weather conditions; case study – Port of Novi Sad, Serbia
- Zircon U–Pb ages of the Paleozoic volcaniclastic strata in the Junggar Basin, NW China
- Monitoring of mangrove forests vegetation based on optical versus microwave data: A case study western coast of Saudi Arabia
- Microfacies analysis of marine shale: A case study of the shales of the Wufeng–Longmaxi formation in the western Chongqing, Sichuan Basin, China
- Multisource remote sensing image fusion processing in plateau seismic region feature information extraction and application analysis – An example of the Menyuan Ms6.9 earthquake on January 8, 2022
- Identification of magnetic mineralogy and paleo-flow direction of the Miocene-quaternary volcanic products in the north of Lake Van, Eastern Turkey
- Impact of fully rotating steel casing bored pile on adjacent tunnels
- Adolescents’ consumption intentions toward leisure tourism in high-risk leisure environments in riverine areas
- Petrogenesis of Jurassic granitic rocks in South China Block: Implications for events related to subduction of Paleo-Pacific plate
- Differences in urban daytime and night block vitality based on mobile phone signaling data: A case study of Kunming’s urban district
- Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan
- Integrated geophysical approach for detection and size-geometry characterization of a multiscale karst system in carbonate units, semiarid Brazil
- Spatial and temporal changes in ecosystem services value and analysis of driving factors in the Yangtze River Delta Region
- Deep fault sliding rates for Ka-Ping block of Xinjiang based on repeating earthquakes
- Improved deep learning segmentation of outdoor point clouds with different sampling strategies and using intensities
- Platform margin belt structure and sedimentation characteristics of Changxing Formation reefs on both sides of the Kaijiang-Liangping trough, eastern Sichuan Basin, China
- Enhancing attapulgite and cement-modified loess for effective landfill lining: A study on seepage prevention and Cu/Pb ion adsorption
- Flood risk assessment, a case study in an arid environment of Southeast Morocco
- Lower limits of physical properties and classification evaluation criteria of the tight reservoir in the Ahe Formation in the Dibei Area of the Kuqa depression
- Evaluation of Viaducts’ contribution to road network accessibility in the Yunnan–Guizhou area based on the node deletion method
- Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
- Element geochemical differences in lower Cambrian black shales with hydrothermal sedimentation in the Yangtze block, South China
- Three-dimensional finite-memory quasi-Newton inversion of the magnetotelluric based on unstructured grids
- Obliquity-paced summer monsoon from the Shilou red clay section on the eastern Chinese Loess Plateau
- Classification and logging identification of reservoir space near the upper Ordovician pinch-out line in Tahe Oilfield
- Ultra-deep channel sand body target recognition method based on improved deep learning under UAV cluster
- New formula to determine flyrock distance on sedimentary rocks with low strength
- Assessing the ecological security of tourism in Northeast China
- Effective reservoir identification and sweet spot prediction in Chang 8 Member tight oil reservoirs in Huanjiang area, Ordos Basin
- Detecting heterogeneity of spatial accessibility to sports facilities for adolescents at fine scale: A case study in Changsha, China
- Effects of freeze–thaw cycles on soil nutrients by soft rock and sand remodeling
- Vibration prediction with a method based on the absorption property of blast-induced seismic waves: A case study
- A new look at the geodynamic development of the Ediacaran–early Cambrian forearc basalts of the Tannuola-Khamsara Island Arc (Central Asia, Russia): Conclusions from geological, geochemical, and Nd-isotope data
- Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region
- Selection of Euler deconvolution solutions using the enhanced horizontal gradient and stable vertical differentiation
- Phase change of the Ordovician hydrocarbon in the Tarim Basin: A case study from the Halahatang–Shunbei area
- Using interpretative structure model and analytical network process for optimum site selection of airport locations in Delta Egypt
- Geochemistry of magnetite from Fe-skarn deposits along the central Loei Fold Belt, Thailand
- Functional typology of settlements in the Srem region, Serbia
- Hunger Games Search for the elucidation of gravity anomalies with application to geothermal energy investigations and volcanic activity studies
- Addressing incomplete tile phenomena in image tiling: Introducing the grid six-intersection model
- Evaluation and control model for resilience of water resource building system based on fuzzy comprehensive evaluation method and its application
- MIF and AHP methods for delineation of groundwater potential zones using remote sensing and GIS techniques in Tirunelveli, Tenkasi District, India
- New database for the estimation of dynamic coefficient of friction of snow
- Measuring urban growth dynamics: A study in Hue city, Vietnam
- Comparative models of support-vector machine, multilayer perceptron, and decision tree predication approaches for landslide susceptibility analysis
- Experimental study on the influence of clay content on the shear strength of silty soil and mechanism analysis
- Geosite assessment as a contribution to the sustainable development of Babušnica, Serbia
- Using fuzzy analytical hierarchy process for road transportation services management based on remote sensing and GIS technology
- Accumulation mechanism of multi-type unconventional oil and gas reservoirs in Northern China: Taking Hari Sag of the Yin’e Basin as an example
- TOC prediction of source rocks based on the convolutional neural network and logging curves – A case study of Pinghu Formation in Xihu Sag
- A method for fast detection of wind farms from remote sensing images using deep learning and geospatial analysis
- Spatial distribution and driving factors of karst rocky desertification in Southwest China based on GIS and geodetector
- Physicochemical and mineralogical composition studies of clays from Share and Tshonga areas, Northern Bida Basin, Nigeria: Implications for Geophagia
- Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
- Research progress of freeze–thaw rock using bibliometric analysis
- Mixed irrigation affects the composition and diversity of the soil bacterial community
- Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
- Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
- Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
- Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
- Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
- Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
- Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
- A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
- Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
- Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
- Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
- Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
- Structural features and tectonic activity of the Weihe Fault, central China
- Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
- Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
- Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
- Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
- Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
- Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
- Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
- Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
- Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
- Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
- Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
- Prediction of formation fracture pressure based on reinforcement learning and XGBoost
- Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
- Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
- Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
- Productive conservation at the landslide prone area under the threat of rapid land cover changes
- Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
- Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
- Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
- Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
- Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
- Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
- Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
- Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
- Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
- Disparities in the geospatial allocation of public facilities from the perspective of living circles
- Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
- Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
- Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
- Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
- Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
- The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
- The critical role of c and φ in ensuring stability: A study on rockfill dams
- Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
- Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
- Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
- Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
- A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
- Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
- Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
- Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
- Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
- Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
- Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
- Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
- Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
- Enhancing the total-field magnetic anomaly using the normalized source strength
- Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
- Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
- Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
- Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
- Tight sandstone fluid detection technology based on multi-wave seismic data
- Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
- Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
- Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
- Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
- Review Articles
- Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
- Prediction and assessment of meteorological drought in southwest China using long short-term memory model
- Communication
- Essential questions in earth and geosciences according to large language models
- Erratum
- Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
- Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
- Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
- Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
- Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
- Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
- Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
- Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
- GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
- Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
- Geosite assessment as the first step for the development of canyoning activities in North Montenegro
- Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
- Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
- Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
- Forest soil CO2 emission in Quercus robur level II monitoring site
- Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
- Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
- Special Issue: Geospatial and Environmental Dynamics - Part I
- Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience