Articles | Volume 18, issue 5
Reviews and syntheses
18 Mar 2021
Reviews and syntheses | 18 Mar 2021
Review and syntheses: Impacts of turbidity flows on deep-sea benthic communities
Katharine T. Bigham et al.
No articles found.
Fabrice Stephenson, Tom Brough, Drew Lohrer, Daniel Leduc, Shane Geange, Owen Anderson, David Bowden, Malcolm R. Clark, Niki Davey, Enrique Pardo, Dennis P. Gordon, Brittany Finucci, Michelle Kelly, Diana Macpherson, Lisa McCartain, Sadie Mills, Kate Neill, Wendy Nelson, Rachael Peart, Matthew H. Pinkerton, Geoffrey B. Read, Jodie Robertson, Ashley Rowden, Kareen Schnabel, Andrew Stewart, Carl Struthers, Leigh Tait, Di Tracey, Shaun Weston, and Carolyn Lundquist
Earth Syst. Sci. Data Discuss.,
Preprint under review for ESSDShort summary
Understanding the distribution of species that live at the seafloor is critical to the management of the marine environment but is lacking in many areas. Here, we showcase an atlas of seafloor biodiversity that describes the distribution of approximately 600 organisms throughout New Zealand’s vast marine realm. Each layer in the open-access atlas has been evaluated by leading experts and provides a key resource for the sustainable use of New Zealand’s marine environment.
Related subject area
Biodiversity and Ecosystem Function: MarineUpwelled plankton community modulates surface bloom succession and nutrient availability in a natural plankton assemblageFirst phytoplankton community assessment of the Kong Håkon VII Hav, Southern Ocean, during austral autumnEarly life stages of a Mediterranean coral are vulnerable to ocean warming and acidificationMediterranean seagrasses as carbon sinks: methodological and regional differencesUnique benthic foraminiferal communities (stained) in diverse environments of sub-Antarctic fjords, South GeorgiaContrasting vertical distributions of recent planktic foraminifera off Indonesia during the southeast monsoon: implications for paleoceanographic reconstructionsThe onset of the spring phytoplankton bloom in the coastal North Sea supports the Disturbance Recovery HypothesisSpecies richness and functional attributes of fish assemblages across a large-scale salinity gradient in shallow coastal areasModeling the growth and sporulation dynamics of the macroalga Ulva in mixed-age populations in cultivation and the formation of green tidesSpatial changes in community composition and food web structure of mesozooplankton across the Adriatic basin (Mediterranean Sea)Predicting mangrove forest dynamics across a soil salinity gradient using an individual-based vegetation model linked with plant hydraulicsWill daytime community calcification reflect reef accretion on future, degraded coral reefs?Modeling polar marine ecosystem functions guided by bacterial physiological and taxonomic traitsQuantifying functional consequences of habitat degradation on a Caribbean coral reefEnhanced chlorophyll-a concentration in the wake of Sable Island, eastern Canada, revealed by two decades of satellite observations: a response to grey seal population dynamics?Population dynamics and reproduction strategies of planktonic foraminifera in the open oceanThe Bouraké semi-enclosed lagoon (New Caledonia) – a natural laboratory to study the lifelong adaptation of a coral reef ecosystem to extreme environmental conditionsAtypical, high-diversity assemblages of foraminifera in a mangrove estuary in northern BrazilPermanent ectoplasmic structures in deep-sea Cibicides and Cibicidoides taxa – long-term observations at in situ pressureIdeas and perspectives: Ushering the Indian Ocean into the UN Decade of Ocean Science for Sustainable Development (UNDOSSD) through marine ecosystem research and operational services – an early career's takePersistent effects of sand extraction on habitats and associated benthic communities in the German BightSpatial patterns of ectoenzymatic kinetics in relation to biogeochemical properties in the Mediterranean Sea and the concentration of the fluorogenic substrate usedA 2-decade (1988–2009) record of diatom fluxes in the Mauritanian coastal upwelling: impact of low-frequency forcing and a two-step shift in the species compositionIdeas and perspectives: When ocean acidification experiments are not the same, repeatability is not testedThe effect of the salinity, light regime and food source on carbon and nitrogen uptake in a benthic foraminiferChanges in population depth distribution and oxygen stratification are involved in the current low condition of the eastern Baltic Sea cod (Gadus morhua)Effects of spatial variability on the exposure of fish to hypoxia: a modeling analysis for the Gulf of MexicoPlant genotype determines biomass response to flooding frequency in tidal wetlandsFactors controlling the competition between Phaeocystis and diatoms in the Southern Ocean and implications for carbon export fluxesCharacterization of particle-associated and free-living bacterial and archaeal communities along the water columns of the South China SeaAdult life strategy affects distribution patterns in abyssal isopods – implications for conservation in Pacific nodule areasDiversity and distribution of nitrogen fixation genes in the oxygen minimum zones of the world oceansStructure and function of epipelagic mesozooplankton and their response to dust deposition events during the spring PEACETIME cruise in the Mediterranean SeaDistribution of planktonic foraminifera in the subtropical South Atlantic: depth hierarchy of controlling factorsTechnical note: Estimating light-use efficiency of benthic habitats using underwater O2 eddy covarianceOcean acidification reduces growth and grazing impact of Antarctic heterotrophic nanoflagellatesDynamics of environmental conditions during the decline of a Cymodocea nodosa meadowMegafauna community assessment of polymetallic-nodule fields with cameras: platform and methodology comparisonA meta-analysis on environmental drivers of marine phytoplankton C : N : PSpatial and temporal variability in the response of phytoplankton and prokaryotes to B-vitamin amendments in an upwelling systemBiogeography and community structure of abyssal scavenging Amphipoda (Crustacea) in the Pacific OceanAre seamounts refuge areas for fauna from polymetallic nodule fields?Ocean deoxygenation and copepods: coping with oxygen minimum zone variabilityUnexpected high abyssal ophiuroid diversity in polymetallic nodule fields of the northeast Pacific Ocean and implications for conservationPopulation dynamics of modern planktonic foraminifera in the western Barents SeaForaminiferal community response to seasonal anoxia in Lake Grevelingen (the Netherlands)Light availability modulates the effects of warming in a marine N2 fixerSiR-actin-labelled granules in foraminifera: patterns, dynamics, and hypothesesAlpha and beta diversity patterns of polychaete assemblages across the nodule province of the eastern Clarion-Clipperton Fracture Zone (equatorial Pacific)Dimensions of marine phytoplankton diversity
Allanah Joy Paul, Lennart Thomas Bach, Javier Arístegui, Elisabeth von der Esch, Nauzet Hernández-Hernández, Jonna Piiparinen, Laura Ramajo, Kristian Spilling, and Ulf Riebesell
Biogeosciences, 19, 5911–5926,Short summary
We investigated how different deep water chemistry and biology modulate the response of surface phytoplankton communities to upwelling in the Peruvian coastal zone. Our results show that the most influential drivers were the ratio of inorganic nutrients (N : P) and the microbial community present in upwelling source water. These led to unexpected and variable development in the phytoplankton assemblage that could not be predicted by the amount of inorganic nutrients alone.
Hanna M. Kauko, Philipp Assmy, Ilka Peeken, Magdalena Różańska-Pluta, Józef M. Wiktor, Gunnar Bratbak, Asmita Singh, Thomas J. Ryan-Keogh, and Sebastien Moreau
Biogeosciences, 19, 5449–5482,Short summary
This article studies phytoplankton (microscopic
plantsin the ocean capable of photosynthesis) in Kong Håkon VII Hav in the Southern Ocean. Different species play different roles in the ecosystem, and it is therefore important to assess the species composition. We observed that phytoplankton blooms in this area are formed by large diatoms with strong silica armors, which can lead to high silica (and sometimes carbon) export to depth and be important prey for krill.
Chloe Carbonne, Steeve Comeau, Phoebe T. W. Chan, Keyla Plichon, Jean-Pierre Gattuso, and Núria Teixidó
Biogeosciences, 19, 4767–4777,Short summary
For the first time, our study highlights the synergistic effects of a 9-month warming and acidification combined stress on the early life stages of a Mediterranean azooxanthellate coral, Astroides calycularis. Our results predict a decrease in dispersion, settlement, post-settlement linear extention, budding and survival under future global change and that larvae and recruits of A. calycularis are stages of interest for this Mediterranean coral resistance, resilience and conservation.
Iris E. Hendriks, Anna Escolano-Moltó, Susana Flecha, Raquel Vaquer-Sunyer, Marlene Wesselmann, and Núria Marbà
Biogeosciences, 19, 4619–4637,Short summary
Seagrasses are marine plants with the capacity to act as carbon sinks due to their high primary productivity, using carbon for growth. This capacity can play a key role in climate change mitigation. We compiled and published data showing that two Mediterranean seagrass species have different metabolic rates, while the study method influences the rates of the measurements. Most communities act as carbon sinks, while the western basin might be more productive than the eastern Mediterranean.
Wojciech Majewski, Witold Szczuciński, and Andrew J. Gooday
Revised manuscript accepted for BGShort summary
We studied foraminifera living in fjords of South Georgia, a sub-Antarctic island sensitive to climate change. As conditions in water and on the seafloor vary, different associations of these microorganisms dominate far inside, in the middle, and near fjord openings. Assemblages in inner and middle parts of fjords are specific to South Georgia but they may become widespread with anticipated warming. These results are important for interpretation of fossil records and monitoring future change.
Raúl Tapia, Sze Ling Ho, Hui-Yu Wang, Jeroen Groeneveld, and Mahyar Mohtadi
Biogeosciences, 19, 3185–3208,Short summary
We report census counts of planktic foraminifera in depth-stratified plankton net samples off Indonesia. Our results show that the vertical distribution of foraminifera species routinely used in paleoceanographic reconstructions varies in hydrographically distinct regions, likely in response to food availability. Consequently, the thermal gradient based on mixed layer and thermocline dwellers also differs for these regions, suggesting potential implications for paleoceanographic reconstructions.
Ricardo González-Gil, Neil S. Banas, Eileen Bresnan, and Michael R. Heath
Biogeosciences, 19, 2417–2426,Short summary
In oceanic waters, the accumulation of phytoplankton biomass in winter, when light still limits growth, is attributed to a decrease in grazing as the mixed layer deepens. However, in coastal areas, it is not clear whether winter biomass can accumulate without this deepening. Using 21 years of weekly data, we found that in the Scottish coastal North Sea, the seasonal increase in light availability triggers the accumulation of phytoplankton biomass in winter, when light limitation is strongest.
Birgit Koehler, Mårten Erlandsson, Martin Karlsson, and Lena Bergström
Biogeosciences, 19, 2295–2312,Short summary
Understanding species richness patterns remains a challenge for biodiversity management. We estimated fish species richness over a coastal salinity gradient (3–32) with a method that allowed comparing data from various sources. Species richness was 3-fold higher at high vs. low salinity, and salinity influenced species’ habitat preference, mobility and feeding type. If climate change causes upper-layer freshening of the Baltic Sea, further shifts along the identified patterns may be expected.
Uri Obolski, Thomas Wichard, Alvaro Israel, Alexander Golberg, and Alexander Liberzon
Biogeosciences, 19, 2263–2271,Short summary
The algal genus Ulva plays a major role in coastal ecosystems worldwide and is a promising prospect as an seagriculture crop. A substantial hindrance to cultivating Ulva arises from sudden sporulation, leading to biomass loss. This process is not yet well understood. Here, we characterize the dynamics of Ulva growth, considering the potential impact of sporulation inhibitors, using a mathematical model. Our findings are an essential step towards understanding the dynamics of Ulva growth.
Emanuela Fanelli, Samuele Menicucci, Sara Malavolti, Andrea De Felice, and Iole Leonori
Biogeosciences, 19, 1833–1851,Short summary
Zooplankton play a key role in marine ecosystems, forming the base of the marine food web and a link between primary producers and higher-order consumers, such as fish. This aspect is crucial in the Adriatic basin, one of the most productive and overexploited areas of the Mediterranean Sea. A better understanding of community and food web structure and their response to water mass changes is essential under a global warming scenario, as zooplankton are sensitive to climate change.
Masaya Yoshikai, Takashi Nakamura, Rempei Suwa, Sahadev Sharma, Rene Rollon, Jun Yasuoka, Ryohei Egawa, and Kazuo Nadaoka
Biogeosciences, 19, 1813–1832,Short summary
This study presents a new individual-based vegetation model to investigate salinity control on mangrove productivity. The model incorporates plant hydraulics and tree competition and predicts unique and complex patterns of mangrove forest structures that vary across soil salinity gradients. The presented model does not hold an empirical expression of salinity influence on productivity and thus may provide a better understanding of mangrove forest dynamics in future climate change.
Coulson A. Lantz, William Leggat, Jessica L. Bergman, Alexander Fordyce, Charlotte Page, Thomas Mesaglio, and Tracy D. Ainsworth
Biogeosciences, 19, 891–906,Short summary
Coral bleaching events continue to drive the degradation of coral reefs worldwide. In this study we measured rates of daytime coral reef community calcification and photosynthesis during a reef-wide bleaching event. Despite a measured decline in coral health across several taxa, there was no change in overall daytime community calcification and photosynthesis. These findings highlight potential limitations of these community-level metrics to reflect actual changes in coral health.
Hyewon Heather Kim, Jeff S. Bowman, Ya-Wei Luo, Hugh W. Ducklow, Oscar M. Schofield, Deborah K. Steinberg, and Scott C. Doney
Biogeosciences, 19, 117–136,Short summary
Heterotrophic marine bacteria are tiny organisms responsible for taking up organic matter in the ocean. Using a modeling approach, this study shows that characteristics (taxonomy and physiology) of bacteria are associated with a subset of ecological processes in the coastal West Antarctic Peninsula region, a system susceptible to global climate change. This study also suggests that bacteria will become more active, in particular large-sized cells, in response to changing climates in the region.
Alice E. Webb, Didier M. de Bakker, Karline Soetaert, Tamara da Costa, Steven M. A. C. van Heuven, Fleur C. van Duyl, Gert-Jan Reichart, and Lennart J. de Nooijer
Biogeosciences, 18, 6501–6516,Short summary
The biogeochemical behaviour of shallow reef communities is quantified to better understand the impact of habitat degradation and species composition shifts on reef functioning. The reef communities investigated barely support reef functions that are usually ascribed to conventional coral reefs, and the overall biogeochemical behaviour is found to be similar regardless of substrate type. This suggests a decrease in functional diversity which may therefore limit services provided by this reef.
Emmanuel Devred, Andrea Hilborn, and Cornelia Elizabeth den Heyer
Biogeosciences, 18, 6115–6132,Short summary
A theoretical model of grey seal seasonal abundance on Sable Island (SI) coupled with chlorophyll-a concentration [chl-a] measured by satellite revealed the impact of seal nitrogen fertilization on the surrounding waters of SI, Canada. The increase in seals from about 100 000 in 2003 to about 360 000 in 2018 during the breeding season is consistent with an increase in [chl-a] leeward of SI. The increase in seal abundance explains 8 % of the [chl-a] increase.
Julie Meilland, Michael Siccha, Maike Kaffenberger, Jelle Bijma, and Michal Kucera
Biogeosciences, 18, 5789–5809,Short summary
Planktonic foraminifera population dynamics has long been assumed to be controlled by synchronous reproduction and ontogenetic vertical migration (OVM). Due to contradictory observations, this concept became controversial. We here test it in the Atlantic ocean for four species of foraminifera representing the main clades. Our observations support the existence of synchronised reproduction and OVM but show that more than half of the population does not follow the canonical trajectory.
Federica Maggioni, Mireille Pujo-Pay, Jérome Aucan, Carlo Cerrano, Barbara Calcinai, Claude Payri, Francesca Benzoni, Yves Letourneur, and Riccardo Rodolfo-Metalpa
Biogeosciences, 18, 5117–5140,Short summary
Based on current experimental evidence, climate change will affect up to 90 % of coral reefs worldwide. The originality of this study arises from our recent discovery of an exceptional study site where environmental conditions (temperature, pH, and oxygen) are even worse than those forecasted for the future. While these conditions are generally recognized as unfavorable for marine life, we found a rich and abundant coral reef thriving under such extreme environmental conditions.
Nisan Sariaslan and Martin R. Langer
Biogeosciences, 18, 4073–4090,Short summary
Analyses of foraminiferal assemblages from the Mamanguape mangrove estuary (northern Brazil) revealed highly diverse, species-rich, and structurally complex biotas. The atypical fauna resembles shallow-water offshore assemblages and are interpreted to be the result of highly saline ocean waters penetrating deep into the estuary. The findings contrast with previous studies, have implications for the fossil record, and provide novel perspectives for reconstructing mangrove environments.
Jutta E. Wollenburg, Jelle Bijma, Charlotte Cremer, Ulf Bickmeyer, and Zora Mila Colomba Zittier
Biogeosciences, 18, 3903–3915,Short summary
Cultured at in situ high-pressure conditions Cibicides and Cibicidoides taxa develop lasting ectoplasmic structures that cannot be retracted or resorbed. An ectoplasmic envelope surrounds their test and may protect the shell, e.g. versus carbonate aggressive bottom water conditions. Ectoplasmic roots likely anchor the specimens in areas of strong bottom water currents, trees enable them to elevate themselves above ground, and twigs stabilize and guide the retractable pseudopodial network.
Biogeosciences, 18, 3631–3635,Short summary
The Indian Ocean Rim hosts many of the underdeveloped and emerging economies that depend on ocean resources for the livelihood of millions. Operational ocean information services cater to the requirements of resource managers and end-users to efficiently harness resources, mitigate threats and ensure safety. This paper outlines existing tools and explores the ongoing research that has the potential to convert the findings into operational services in the near- to midterm.
Finn Mielck, Rune Michaelis, H. Christian Hass, Sarah Hertel, Caroline Ganal, and Werner Armonies
Biogeosciences, 18, 3565–3577,Short summary
Marine sand mining is becoming more and more important to nourish fragile coastlines that face global change. We investigated the largest sand extraction site in the German Bight. The study reveals that after more than 35 years of mining, the excavation pits are still detectable on the seafloor while the sediment composition has largely changed. The organic communities living in and on the seafloor were strongly decimated, and no recovery is observable towards previous conditions.
France Van Wambeke, Elvira Pulido, Philippe Catala, Julie Dinasquet, Kahina Djaoudi, Anja Engel, Marc Garel, Sophie Guasco, Barbara Marie, Sandra Nunige, Vincent Taillandier, Birthe Zäncker, and Christian Tamburini
Biogeosciences, 18, 2301–2323,Short summary
Michaelis–Menten kinetics were determined for alkaline phosphatase, aminopeptidase and β-glucosidase in the Mediterranean Sea. Although the ectoenzymatic-hydrolysis contribution to heterotrophic prokaryotic needs was high in terms of N, it was low in terms of C. This study points out the biases in interpretation of the relative differences in activities among the three tested enzymes in regard to the choice of added concentrations of fluorogenic substrates.
Oscar E. Romero, Simon Ramondenc, and Gerhard Fischer
Biogeosciences, 18, 1873–1891,Short summary
Upwelling intensity along NW Africa varies on the interannual to decadal timescale. Understanding its changes is key for the prediction of future changes of CO2 sequestration in the northeastern Atlantic. Based on a multiyear (1988–2009) sediment trap experiment at the site CBmeso, fluxes and the species composition of the diatom assemblage are presented. Our data help in establishing the scientific basis for forecasting and modeling future states of this ecosystem and its decadal changes.
Phillip Williamson, Hans-Otto Pörtner, Steve Widdicombe, and Jean-Pierre Gattuso
Biogeosciences, 18, 1787–1792,Short summary
The reliability of ocean acidification research was challenged in early 2020 when a high-profile paper failed to corroborate previously observed impacts of high CO2 on the behaviour of coral reef fish. We now know the reason why: the
replicatedstudies differed in many ways. Open-minded and collaborative assessment of all research results, both negative and positive, remains the best way to develop process-based understanding of the impacts of ocean acidification on marine organisms.
Michael Lintner, Bianca Lintner, Wolfgang Wanek, Nina Keul, and Petra Heinz
Biogeosciences, 18, 1395–1406,Short summary
Foraminifera are unicellular marine organisms that play an important role in the marine element cycle. Changes of environmental parameters such as salinity or temperature have a significant impact on the faunal assemblages. Our experiments show that changes in salinity immediately influence the foraminiferal activity. Also the light regime has a significant impact on carbon or nitrogen processing in foraminifera which contain no kleptoplasts.
Michele Casini, Martin Hansson, Alessandro Orio, and Karin Limburg
Biogeosciences, 18, 1321–1331,Short summary
In the past 20 years the condition of the eastern Baltic cod has dropped, with large implications for the fishery. Our results show that simultaneously the cod population has moved deeper while low-oxygenated waters detrimental for cod growth have become shallower. Cod have thus dwelled more in detrimental waters, explaining the drop in its condition. This study, using long-term fish and hydrological monitoring data, evidences the impact of deoxygenation on fish biology and fishing.
Elizabeth D. LaBone, Kenneth A. Rose, Dubravko Justic, Haosheng Huang, and Lixia Wang
Biogeosciences, 18, 487–507,Short summary
The hypoxic zone is an area of low dissolved oxygen (DO) in the Gulf of Mexico. Fish can be killed by exposure to hypoxia and can be negatively impacted by exposure to low, nonlethal DO concentrations (sublethal DO). We found that high sublethal area resulted in higher exposure and DO variability had a small effect on exposure. There was a large variation in exposure among individuals, which when combined with spatial variability of DO, can result in an underestimation of exposure when averaged.
Svenja Reents, Peter Mueller, Hao Tang, Kai Jensen, and Stefanie Nolte
Biogeosciences, 18, 403–411,Short summary
By conducting a flooding experiment with two genotypes of the salt-marsh grass Elymus athericus, we show considerable differences in biomass response to flooding within the same species. As biomass production plays a major role in sedimentation processes and thereby salt-marsh accretion, we emphasise the importance of taking intraspecific differences into account when evaluating ecosystem resilience to accelerated sea level rise.
Cara Nissen and Meike Vogt
Biogeosciences, 18, 251–283,Short summary
Using a regional Southern Ocean ecosystem model, we find that the relative importance of Phaeocystis and diatoms at high latitudes is controlled by iron and temperature variability, with light levels controlling the seasonal succession in coastal areas. Yet, biomass losses via aggregation and grazing matter as well. We show that the seasonal succession of Phaeocystis and diatoms impacts the seasonality of carbon export fluxes with ramifications for nutrient cycling and food web dynamics.
Jiangtao Li, Lingyuan Gu, Shijie Bai, Jie Wang, Lei Su, Bingbing Wei, Li Zhang, and Jiasong Fang
Biogeosciences, 18, 113–133,Short summary
Few studies have focused on the particle-attached (PA) and free-living (FL) microbes of the deep ocean. Here we determined PA and FL microbial communities along depth profiles of the SCS. PA and FL fractions accommodated divergent microbial compositions, and most of them are potentially generalists with PA and FL dual lifestyles. A potential vertical connectivity between surface-specific microbes and those in the deep ocean was indicated, likely through microbial attachment to sinking particles.
Saskia Brix, Karen J. Osborn, Stefanie Kaiser, Sarit B. Truskey, Sarah M. Schnurr, Nils Brenke, Marina Malyutina, and Pedro Martinez Arbizu
Biogeosciences, 17, 6163–6184,Short summary
The Clarion–Clipperton Fracture Zone (CCZ) located in the Pacific is commercially the most important area of proposed manganese nodule mining. Extraction of this will influence the life and distribution of small deep-sea invertebrates like peracarid crustaceans, of which >90 % are undescribed species new to science. We are doing a species delimitation approach as baseline for an ecological interpretation of species distribution and discuss the results in light of future deep-sea conservation.
Amal Jayakumar and Bess B. Ward
Biogeosciences, 17, 5953–5966,Short summary
Diversity and community composition of nitrogen-fixing microbes in the three main oxygen minimum zones of the world ocean were investigated using nifH clone libraries. Representatives of three main clusters of nifH genes were detected. Sequences were most diverse in the surface waters. The most abundant OTUs were affiliated with Alpha- and Gammaproteobacteria. The sequences were biogeographically distinct and the dominance of a few OTUs was commonly observed in OMZs in this (and other) studies.
Guillermo Feliú, Marc Pagano, Pamela Hidalgo, and François Carlotti
Biogeosciences, 17, 5417–5441,Short summary
The impact of Saharan dust deposition events on the Mediterranean Sea ecosystem was studied during a basin-scale survey (PEACETIME cruise, May–June 2017). Short-term responses of the zooplankton community were observed after episodic dust deposition events, highlighting the impact of these events on productivity up to the zooplankton level in the poorly fertilized pelagic ecosystems of the southern Mediterranean Sea.
Douglas Lessa, Raphaël Morard, Lukas Jonkers, Igor M. Venancio, Runa Reuter, Adrian Baumeister, Ana Luiza Albuquerque, and Michal Kucera
Biogeosciences, 17, 4313–4342,Short summary
We observed that living planktonic foraminifera had distinct vertically distributed communities across the Subtropical South Atlantic. In addition, a hierarchic alternation of environmental parameters was measured to control the distribution of planktonic foraminifer's species depending on the water depth. This implies that not only temperature but also productivity and subsurface processes are signed in fossil assemblages, which could be used to perform paleoceanographic reconstructions.
Karl M. Attard and Ronnie N. Glud
Biogeosciences, 17, 4343–4353,Short summary
Light-use efficiency defines the ability of primary producers to convert sunlight energy to primary production. This report provides a framework to compute hourly and daily light-use efficiency using underwater eddy covariance, a recent technological development that produces habitat-scale rates of primary production for many different habitat types. The approach, tested on measured flux data, provides a useful means to compare habitat productivity across time and space.
Stacy Deppeler, Kai G. Schulz, Alyce Hancock, Penelope Pascoe, John McKinlay, and Andrew Davidson
Biogeosciences, 17, 4153–4171,Short summary
Our study showed how ocean acidification can exert both direct and indirect influences on the interactions among trophic levels within the microbial loop. Microbial grazer abundance was reduced at CO2 concentrations at and above 634 µatm, while microbial communities increased in abundance, likely due to a reduction in being grazed. Such changes in predator–prey interactions with ocean acidification could have significant effects on the food web and biogeochemistry in the Southern Ocean.
Mirjana Najdek, Marino Korlević, Paolo Paliaga, Marsej Markovski, Ingrid Ivančić, Ljiljana Iveša, Igor Felja, and Gerhard J. Herndl
Biogeosciences, 17, 3299–3315,Short summary
The response of Cymodocea nodosa to environmental changes was reported during a 15-month period. The meadow decline was triggered in spring by the simultaneous reduction of available light in the water column and the creation of anoxic conditions in the rooted area. This disturbance was critical for the plant since it took place during its recruitment phase when metabolic needs are maximal and stored reserves minimal. The loss of such habitat-forming seagrass is a major environmental concern.
Timm Schoening, Autun Purser, Daniel Langenkämper, Inken Suck, James Taylor, Daphne Cuvelier, Lidia Lins, Erik Simon-Lledó, Yann Marcon, Daniel O. B. Jones, Tim Nattkemper, Kevin Köser, Martin Zurowietz, Jens Greinert, and Jose Gomes-Pereira
Biogeosciences, 17, 3115–3133,Short summary
Seafloor imaging is widely used in marine science and industry to explore and monitor areas of interest. The selection of the most appropriate imaging gear and deployment strategy depends on the target application. This paper compares imaging platforms like autonomous vehicles or towed camera frames and different deployment strategies of those in assessing the megafauna abundance of polymetallic-nodule fields. The deep-sea mining industry needs that information for robust impact monitoring.
Tatsuro Tanioka and Katsumi Matsumoto
Biogeosciences, 17, 2939–2954,Short summary
We conducted an extensive literature survey (meta-analysis) on how the C : N : P ratio varies with change in key environmental drivers. We found that the expected reduction in nutrients and warming under the future climate change scenario is likely to result in increased C : P and C : N of marine phytoplankton. Further, our findings highlight the greater stoichiometric plasticity of eukaryotes over prokaryotes, which provide us insights on how to understand and model plankton.
Vanessa Joglar, Antero Prieto, Esther Barber-Lluch, Marta Hernández-Ruiz, Emilio Fernández, and Eva Teira
Biogeosciences, 17, 2807–2823,Short summary
Coastal marine ecosystems are among the most ecologically and economically productive areas providing a large fraction of ecosystem goods and services to human populations, and B vitamins have long been considered important growth factors for phytoplankton. Our findings indicate that the responses of microbial plankton to B-vitamin supply are mainly driven by the bacterial community composition and that microbial plankton in this area seems to be well adapted to cope with B-vitamin shortage.
Tasnim Patel, Henri Robert, Cedric D'Udekem D'Acoz, Koen Martens, Ilse De Mesel, Steven Degraer, and Isa Schön
Biogeosciences, 17, 2731–2744,Short summary
Exploitation of deep-sea resources in one of the largest ecosystems on the planet has rendered research of its biodiversity more urgent than ever before. We investigated the known habitats and connectivity of deep-sea scavenging amphipods and obtained important knowledge about several species. We also demonstrated that a long-term disturbance experiment has possibly reduced amphipod biodiversity. These data and further sampling expeditions are instrumental for formulating sustainable policies.
Daphne Cuvelier, Pedro A. Ribeiro, Sofia P. Ramalho, Daniel Kersken, Pedro Martinez Arbizu, and Ana Colaço
Biogeosciences, 17, 2657–2680,Short summary
Polymetallic nodule mining will remove hard substrata from the abyssal deep-sea floor. The only neighbouring ecosystems featuring hard substratum are seamounts, and their inhabiting fauna could aid in recovery post-mining. Nevertheless, first observations of seamount megafauna were very different from nodule-associated megafauna and showed little overlap. The possible uniqueness of these ecosystems implies that they should be included in management plans for the conservation of biodiversity.
Karen F. Wishner, Brad Seibel, and Dawn Outram
Biogeosciences, 17, 2315–2339,Short summary
Increasing deoxygenation and oxygen minimum zone expansion are consequences of global warming. Copepod species had different vertical distribution strategies and physiologies associated with oxygen profile variability (0–1000 m). Species (1) changed vertical distributions and maximum abundance depth, (2) shifted diapause depth, (3) changed diel vertical migration depths, or (4) changed epipelagic depth range in the aerobic mixed layer. Present-day variability helps predict future scenarios.
Magdalini Christodoulou, Timothy O'Hara, Andrew F. Hugall, Sahar Khodami, Clara F. Rodrigues, Ana Hilario, Annemiek Vink, and Pedro Martinez Arbizu
Biogeosciences, 17, 1845–1876,Short summary
Unexpectedly high diversity was revealed in areas licenced for polymetallic nodule mining exploration in the Pacific Ocean. For the first time, a comprehensive reference library including 287 novel ophiuroid sequences allocated to 43 species was produced. Differences in food availability along the nodule province of CCZ were reflected in the biodiversity patterns observed. The APEI3's dissimilarity with the exploration contract areas questions its ability to serve as a biodiversity reservoir.
Julie Meilland, Hélène Howa, Vivien Hulot, Isaline Demangel, Joëlle Salaün, and Thierry Garlan
Biogeosciences, 17, 1437–1450,Short summary
This study reports on planktonic foraminifera (PF) diversity and distribution in the Barents Sea. The species Globigerinita uvula and Turborotalita quinqueloba dominate the water column while surface sediments are dominated by Neogloboquadrina pachyderma. We hypothesize the unusual dominance of G. uvula in the water to be a seasonal signal or a result of climate forcing. Size-normalized-protein concentrations of PF show a northward decrease, suggesting biomass to vary with the environment.
Julien Richirt, Bettina Riedel, Aurélia Mouret, Magali Schweizer, Dewi Langlet, Dorina Seitaj, Filip J. R. Meysman, Caroline P. Slomp, and Frans J. Jorissen
Biogeosciences, 17, 1415–1435,Short summary
The paper presents the response of benthic foraminiferal communities to seasonal absence of oxygen coupled with the presence of hydrogen sulfide, considered very harmful for several living organisms. Our results suggest that the foraminiferal community mainly responds as a function of the duration of the adverse conditions. This knowledge is especially useful to better understand the ecology of benthic foraminifera but also in the context of palaeoceanographic interpretations.
Xiangqi Yi, Fei-Xue Fu, David A. Hutchins, and Kunshan Gao
Biogeosciences, 17, 1169–1180,Short summary
Combined effects of warming and light intensity were estimated in N2-fixing cyanobacterium Trichodesmium. Its physiological responses to warming were significantly modulated by light, with growth peaking at 27 °C under the light-saturating condition but being non-responsive across the range of 23–31 °C under the light-limiting condition. Light shortage also weakened the acclimation ability of Trichodesmium to warming, making light-limited Trichodesmium more sensitive to acute temperature change.
Jan Goleń, Jarosław Tyszka, Ulf Bickmeyer, and Jelle Bijma
Biogeosciences, 17, 995–1011,Short summary
We studied the organisation and dynamics of actin in foraminifera. Actin is one of the key structural proteins in most lifeforms. Our investigations show that in foraminifera it forms small granules, around 1 µm in diameter, that display rapid movement. This granularity is unusual in comparison to other organisms. We suppose that these granules are most likely involved in the formation of all types of pseudopods responsible for movement, food capturing, biomineralisation, and other functions.
Paulo Bonifácio, Pedro Martínez Arbizu, and Lénaïck Menot
Biogeosciences, 17, 865–886,Short summary
The patterns observed in the composition of polychaete assemblages were attributed to variations in food supply at the regional scale and nodule density at the local scale. The high levels of species replacement were mainly driven by rare species, leading to regional species pool estimates between 498 and 240 000 species. The high proportion of singletons seems reflect an under-sampling bias that is currently preventing the assessment of potential biodiversity loss due to nodule mining.
Stephanie Dutkiewicz, Pedro Cermeno, Oliver Jahn, Michael J. Follows, Anna E. Hickman, Darcy A. A. Taniguchi, and Ben A. Ward
Biogeosciences, 17, 609–634,Short summary
Phytoplankton are an essential component of the marine food web and earth's carbon cycle. We use observations, ecological theory and a unique trait-based ecosystem model to explain controls on patterns of marine phytoplankton biodiversity. We find that different dimensions of diversity (size classes, biogeochemical functional groups, thermal norms) are controlled by a disparate combination of mechanisms. This may explain why previous studies of phytoplankton diversity had conflicting results.
Aller, J. Y.: Benthic community response to temporal and spatial gradients in physical disturbance within a deep-sea western boundary region, Deep Sea Res. Part I Oceanogr. Res. Pap., 44, 39–69, https://doi.org/10.1016/S0967-0637(96)00092-1, 1997.
Angel, M. V. and Rice, T. L.: The ecology of the deep ocean and its relevance to global waste management, J. Appl. Ecol., 33, 915–926, https://doi.org/10.2307/2404673, 1996.
Anschutz, P., Jorissen, F. J., Chaillou, G., Abu-Zied, R., and Fontanier, C.: Recent turbidite deposition in the eastern Atlantic: Early diagenesis and biotic recovery, J. Mar. Res., 60, 835–854, https://doi.org/10.1357/002224002321505156, 2002.
Bao, R., Strasser, M., McNichol, A. P., Haghipour, N., McIntyre, C., Wefer, G., and Eglinton, T. I.: Tectonically-triggered sediment and carbon export to the Hadal zone, Nat. Commun., 9, 1–8, https://doi.org/10.1038/s41467-017-02504-1, 2018.
Bender, E. A., Case, T. J., and Gilpin, M. E.: Perturbation Experiments in Community Ecology: Theory and Practice, Ecology, 65, 1–13, https://doi.org/10.2307/1939452, 1984.
Briggs, K. B., Richardson, M. D., and Young, D. K.: Variability in geoacoustic and related properties of surface sediments from the Venezuela Basin, Caribbean Sea, Mar. Geol., 68, 73–106, https://doi.org/10.1016/0025-3227(85)90006-4, 1985.
Briggs, K. B., Richardson, M. D., and Young, D. K.: The classification and structure of megafaunal assemblages in the Venezuela Basin, Caribbean Sea, J. Mar. Res., 54, 705–730, https://doi.org/10.1357/0022240963213736, 1996.
Carey, A. G.: A comparison of benthic infaunal abundance on two abyssal plains in the northeast Pacific Ocean, Deep Sea Res. Part I Oceanogr. Res. Pap., 28, 467–479, https://doi.org/10.1016/0198-0149(81)90138-2, 1981.
Carman, K. R., Sherman, K. M., and Thistle, D.: Evidence that sediment type influences the horizontal and vertical distribution of nematodes at a deep-sea site, Deep Sea Res. Part I Oceanogr. Res. Pap., 34, 45–53, https://doi.org/10.1016/0198-0149(87)90120-8, 1987.
Carter, L., Milliman, J. D., Talling, P. J., Gavey, R., and Wynn, R. B.: Near-synchronous and delayed initiation of long run-out submarine sediment flows from a record-breaking river flood, offshore Taiwan, Geophys. Res. Lett., 39, 6–10, https://doi.org/10.1029/2012GL051172, 2012.
Carter, L., Gavey, R., Talling, P. J., and Liu, J. T.: Insights into submarine geohazards from breaks in subsea telecommunication cables, Oceanography, 27, 58–67, https://doi.org/10.5670/oceanog.2014.40, 2014.
Churchill, E. D. and Hanson, H. C.: The concept of climax in arctic and alpine vegetation, Bot. Rev., 24, 127–191, https://doi.org/10.1007/BF02872544, 1958.
Cole, K. H., Guinasso, N. L., Richardson, M. D., Johnson, J. W., and Schink, D. R.: Uranium and thorium series isotopes in recent sediments of the Venezuela Basin, Caribbean Sea, Mar. Geol., 68, 167–185, https://doi.org/10.1016/0025-3227(85)90010-6, 1985.
Collie, J. S., Escanero, G. A., and Valentine, P. C.: Photographic evaluation of the impacts of bottom fishing on benthic epifauna, ICES J. Mar. Sci., 57, 987–1001, https://doi.org/10.1006/jmsc.2000.0584, 2000.
Crandall, R. M., Hayes, C. R., and Ackland, E. N.: Application of the intermediate disturbance hypothesis to flooding, Community Ecol., 4, 225–232, https://doi.org/10.1556/ComEc.4.2003.2.9, 2003.
Dayton, P. K.: Competition, Disturbance, and Community Organization: The Provision and Subsequent Utilization of Space in a Rocky Intertidal Community, Ecological Society of America, Ecol. Monogr., 41, 351–389, 1971.
De Leo, F. C., Smith, C. R., Rowden, A. A., Bowden, D. A., and Clark, M. R.: Submarine canyons: Hotspots of benthic biomass and productivity in the deep sea, Proc. R. Soc. B, 277, 2783–2792, https://doi.org/10.1098/rspb.2010.0462, 2010.
Dennielou, B., Droz, L., Babonneau, N., Jacq, C., Bonnel, C., Picot, M., Le Saout, M., Saout, Y., Bez, M., Savoye, B., Olu, K., and Rabouille, C.: Morphology, structure, composition and build-up processes of the active channel-mouth lobe complex of the Congo deep-sea fan with inputs from remotely operated underwater vehicle (ROV) multibeam and video surveys, Deep Sea Res. Part II Top. Stud. Oceanogr., 142, 25–49, https://doi.org/10.1016/j.dsr2.2017.03.010, 2017.
Dial, R. and Roughgarden, J.: Theory of marine communities: The intermediate disturbance hypothesis, Ecology, 79, 1412–1424, https://doi.org/10.1890/0012-9658(1998)079[1412:TOMCTI]2.0.CO;2, 1998.
Embley, R. W., Eittreim, S. L., McHugh, C. H., Normark, W. R., Rau, G. H., Hecker, B., DeBevoise, A. E., Greene, H. G., Ryan, W. B. F., Harrold, C., and Baxter, C.: Geological setting of chemosynthetic communities in the Monterey Fan Valley system, Deep Sea Res. Part I Oceanogr. Res. Pap., 37, 1651–1667, https://doi.org/10.1016/0198-0149(90)90069-8, 1990.
Etter, R. J. and Grassle, J. F.: Patterns of species diversity in the deep sea as a function of sediment particle size diversity, Nature, 360, 576–578, https://doi.org/10.1038/360576a0, 1992.
Folke, C., Carpenter, S., Walker, B., Scheffer, M., Elmqvist, T., Gunderson, L., and Holling, C. S.: Regime shifts, resilience, and biodiversity in ecosystem management, Annu. Rev. Ecol. Evol. Syst., 35, 557–581, https://doi.org/10.1146/annurev.ecolsys.35.021103.105711, 2004.
Froelich, P. N., Klinkhammer, G. P., Bender, M. L., Luedtke, N. A., Heath, G. R., Cullen, D., Dauphin, P., Hammond, D., Hartman, B., and Maynard, V.: Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis, Geochim. Cosmochim. Acta, 43, 1075–1090, https://doi.org/10.1016/0016-7037(79)90095-4, 1979.
Frutos, I. and Sorbe, J. C.: Suprabenthic assemblages from the Capbreton area (SE Bay of Biscay). Faunal recovery after a canyon turbidity disturbance, Deep Sea Res. Part I Oceanogr. Res. Pap., 130, 36–46, https://doi.org/10.1016/j.dsr.2017.10.007, 2017.
Galéron, J., Menot, L., Renaud, N., Crassous, P., Khripounoff, A., Treignier, C., and Sibuet, M.: Spatial and temporal patterns of benthic macrofaunal communities on the deep continental margin in the Gulf of Guinea, Deep Sea Res. Part II Top. Stud. Oceanogr., 56, 2299–2312, https://doi.org/10.1016/j.dsr2.2009.04.011, 2009.
Glover, A., Paterson, G., Bett, B., Gage, J., Myriam Sibuet, Sheader, M., and Hawkins, L.: Patterns in polychaete abundance and diversity from the Madeira Abyssal Plain, northeast Atlantic, Deep Sea Res. Part I Oceanogr. Res. Pap., 48, 217–236, https://doi.org/10.1016/S0967-0637(00)00053-4, 2001.
Glover, A. G., Gooday, A. J., Bailey, D. M., Billett, D. S. M., Chevaldonné, P., Colaço, A., Copley, J., Cuvelier, D., Desbruyères, D., Kalogeropoulou, V., Klages, M., Lampadariou, N., Lejeusne, C., Mestre, N. C., Paterson, G. L. J., Perez, T., Ruhl, H., Sarrazin, J., Soltwedel, T., Soto, E. H., Thatje, S., Tselepides, A., Van Gaever, S., and Vanreusel, A.: Temporal Change in Deep-Sea Benthic Ecosystems. A Review of the Evidence From Recent Time-Series Studies, Adv. Mar. Biol., 58, 1–95, https://doi.org/10.1016/B978-0-12-381015-1.00001-0, 2010.
Gooday, A. J.: Epifaunal and shallow infaunal foraminiferal communities at three abyssal NE Atlantic sites subject to differing phytodetritus input regimes, Deep Sea Res. Part I Oceanogr. Res. Pap., 43, 1395–1421, https://doi.org/10.1016/S0967-0637(96)00072-6, 1996.
Gooday, A. J., Turley, C. M., and Allen, J. A.: Responses by Benthic Organisms to Inputs of Organic Material to the Ocean Floor: A Review, Philos. Trans. Roy. Soc. A, 331, 119–138, https://doi.org/10.1098/rsta.1990.0060, 1990.
Gorsline, D. S.: Deep-water sedimentologic conditions and models, Mar. Geol., 38, 1–21, https://doi.org/10.1016/0025-3227(80)90049-3, 1980.
Griggs, G. B. and Kulm, L. D.: Sedimentation in Cascadia Deep-Sea Channel, Geol. Soc. Am. Bull., 81, 1361–1384, https://doi.org/10.1130/0016-7606(1970)81[1361:SICDC]2.0.CO;2, 1970.
Griggs, G. B., Carey, A. G., and Kulm, L. D.: Deep-sea sedimentation and sediment-fauna interaction in Cascadia Channel and on Cascadia Abyssal Plain, Deep Sea Res. Oceanogr. Abstr., 16, 157–170, https://doi.org/10.1016/0011-7471(69)90071-0, 1969.
Hall, S. J.: Physical disturbance and marine benthic communities Life in unconsolidated sediments, edited by A. D. Ansell, R. N. Gibson, and M. Barnes, Oceanogr. Mar. Biol. Annu. Rev., 32, 179–239, 1994.
Hall, S. J., Raffaelli, D., and Thrush, S. F.: Patchiness and Disturbance in Shallow Water Benthic Assemblages, Aquat. Ecol., 34, 333–375, 1994.
Harris, P. T.: Shelf and deep-sea sedimentary environments and physical benthic disturbance regimes: A review and synthesis, Mar. Geol., 353, 169–184, https://doi.org/10.1016/j.margeo.2014.03.023, 2014.
Heerema, C. J., Talling, P. J., Cartigny, M. J., Paull, C. K., Bailey, L., Simmons, S. M., Parsons, D. R., Clare, M. A., Gwiazda, R., Lundsten, E., Anderson, K., Maier, K. L., Xu, J. P., Sumner, E. J., Rosenberger, K., Gales, J., McGann, M., Carter, L., and Pope, E.: What determines the downstream evolution of turbidity currents?, Earth Planet. Sci. Lett., 532, 116023, https://doi.org/10.1016/j.epsl.2019.116023, 2020.
Heezen, B. C. and Ewing, M.: Turbidity currents and submarine slumps, and the 1929 Grand Banks earthquake, Am. J. Sci., 250, 849–873, 1952.
Heezen, B. C., Ewing, M., and Menzies, R. J.: The influence of submarine turbidity currents on abyssal productivity, Oikos, 170–182, 1955.
Heezen, B. C., Menzies, R. J., Schneider, E. D., Ewing, M. and Granelli, N. C. L.: Congo Submarine Canyon, AAPG Bull., 48, https://doi.org/10.1306/BC743D7F-16BE-11D7-8645000102C1865D, 1964.
Hess, S. and Jorissen, F. J.: Distribution patterns of living benthic foraminifera from Cap Breton canyon, Bay of Biscay: Faunal response to sediment instability, Deep Sea Res. Part I Oceanogr. Res. Pap., 56, 1555–1578, https://doi.org/10.1016/j.dsr.2009.04.003, 2009.
Hess, S., Jorrissen, F. J., Venet, V., and Abu-Zied, R.: Benthic Foraminiferal Recovery After Recent Turbidite Deposition in Cap Breton Canyon, Bay of Biscay, J. Foraminiferal Res., 35, 114–129, https://doi.org/10.2113/35.2.114, 2005.
Holling, C. S.: Engineering Resilience versus Ecological Resilience, in: Foundations of Ecological Resilence, National Academy of Engineering, Washington, DC, 31–44, 1996.
Honjo, S. and Manganini, S. J.: Annual biogenic particle fluxes to the interior of the North Atlantic Ocean; studied at 34∘ N 21∘ W and 48∘ N 21∘ W, Deep Sea Res. Part II Top. Stud. Oceanogr., 40, 587–607, https://doi.org/10.1016/0967-0645(93)90034-K, 1993.
Hsu, S.-K., Kuo, J., Lo, C.-L., Tsai, C.-H., Doo, W.-B., Ku, C.-Y., and Sibuet, J.-C.: Turbidity Currents, Submarine Landslides and the 2006 Pingtung Earthquake off SW Taiwan, Terr. Atmos. Ocean. Sci., 19, 767, https://doi.org/10.3319/TAO.2008.19.6.767(PT), 2008.
Huggett, Q. J.: Mapping the hemipelagic versus turbiditic muds by feeding traces observed in deep-sea photographs, Geol. Geochemistry Abyssal Plains, Geol. Soc. Spec. Publ., 31, 105–112, 1987.
Hughes Clarke, J., Shor, A. N., Piper, D. J. W., and Mayer, L. A.: Large-scale current induced erosion and deposition in the path of the 1929 Grand Banks Turbidity current, Sedimentology, 37, 613–629, 1990.
Hyacinthe, C., Anschutz, P., Carbonel, P., Jouanneau, J.-M., and Jorrisen, F. J.: Early diagentic processes in the muddy sediments of the Bay of Biscay, Mar. Geol. 177, 111–128, https://doi.org/10.1016/S0025-3227(01)00127-X, 2001.
Jahnke, R. A. and Jackson, G. A.: The Spatial Distribution of Sea Floor Oxygen Consumption in The Atlantic and Pacific Oceans, in: Deep-Sea Food Chains and the Global Carbon Cycle, pp. 295–307, Springer, the Netherlands, Dordrecht, 1992.
Jumars, P. A.: Limits in Predicting and Detecting Benthic Community Responses to Manganese Nodule Mining, Mar. Min, 3, 213–229, 1981.
Kasaya, T., Mitsuzawa, K., Goto, T. nori, Iwase, R., Sayanagi, K., Araki, E., Asakawa, K., Mikada, H., Watanabe, T., Takahashi, I., and Nagao, T.: Trial of multidisciplinary observation at an expandable sub-marine cabled station “Off-Hatsushima Island Observatory” in Sagami Bay, Japan, Sensors, 9, 9241–9254, https://doi.org/10.3390/s91109241, 2009.
Kawagucci, S., Yoshida, Y. T., Noguchi, T., Honda, M. C., Uchida, H., Ishibashi, H., Nakagawa, F., Tsunogai, U., Okamura, K., Takaki, Y., Nunoura, T., Miyazaki, J., Hirai, M., Lin, W., Kitazato, H., and Takai, K.: Disturbance of deep-sea environments induced by the M9.0 Tohoku Earthquake, Sci. Rep., 2, 1–7, https://doi.org/10.1038/srep00270, 2012.
Khripounoff, A., Vangriesheim, A., Babonneau, N., Crassous, P., Dennielou, B., and Savoye, B.: Direct observation of intense turbidity current activity in the Zaire submarine valley at 4000 m water depth, Mar. Geol., 194, 151–158, https://doi.org/10.1016/S0025-3227(02)00677-1, 2003.
Kioka, A., Schwestermann, T., Moernaut, J., Ikehara, K., Kanamatsu, T., McHugh, C. M., dos Santos Ferreira, C., Wiemer, G., Haghipour, N., Kopf, A. J., Eglinton, T. I., and Strasser, M.: Megathrust earthquake drives drastic organic carbon supply to the hadal trench, Sci. Rep., 9, 1–10, https://doi.org/10.1038/s41598-019-38834-x, 2019.
Kitahashi, T., Jenkins, R. G., Nomaki, H., Shimanaga, M., Fujikura, K., and Kojima, S.: Effect of the 2011 Tohoku Earthquake on deep-sea meiofaunal assemblages inhabiting the landward slope of the Japan Trench, Mar. Geol., 358, 128–137, https://doi.org/10.1016/j.margeo.2014.05.004, 2014.
Kitahashi, T., Watanabe, H., Ikehara, K., Jenkins, R. G., Kojima, S., and Shimanaga, M.: Deep-sea meiofauna off the Pacific coast of Tohoku and other trench slopes around Japan: a comparative study before and after the 2011 off the Pacific coast of Tohoku Earthquake, J. Oceanogr., 72, 129–139, https://doi.org/10.1007/s10872-015-0323-3, 2016.
Kitahashi, T., Jenkins, R. G., Kojima, S., and Shimanaga, M.: High resilience of harpacticoid copepods in the landward slope of the Japan Trench against disturbance of the 2011 Tohoku Earthquake, Limnol. Oceanogr., 63, 2751–2761, https://doi.org/10.1002/lno.11006, 2018.
Kranz, P. M.: The Anastrophic Burial of Bivalves and its Paleoecological Significance, J. Geol., 82, 237–265, https://doi.org/10.1086/627961, 1974.
Kuenen, P. H. and Migliorini, C. I.: Turbidity currents as a cause of graded bedding, J. Geol., 58, 91–127, 1950.
Lambshead, P. J. D., Ferrero, T. J., and Wollf, G. A.: Comparison of the Vertical Distribution of Nematodes from Two Contrasting Abyssal Sites in the Northeast Atlantic Subject to Different Seasonal Inputs of Phytodetritus, Int. Rev. ges. Hydrobiol. Hydrogr., 80, 327–331, https://doi.org/10.1002/iroh.19950800219, 1995.
Lambshead, P. J. D., Tietjen, J. H., Glover, A., Ferrero, T., Thistle, D., and Gooday, A. J.: Impact of large-scale natural physical disturbance on the diversity of deep-sea North Atlantic nematodes, Mar. Ecol. Prog. Ser., 214, 121–126, https://doi.org/10.3354/meps214121, 2001.
Leduc, D., Rowden, A. A., Probert, P. K., Pilditch, C. A., Nodder, S. D., Vanreusel, A., Duineveld, G. C. A., and Witbaard, R.: Further evidence for the effect of particle-size diversity on deep-sea benthic biodiversity, Deep Sea Res. Part I Oceanogr. Res. Pap., 63, 164–169, https://doi.org/10.1016/j.dsr.2011.10.009, 2012.
Leduc, D., Rowden, A. A., Nodder, S. D., Berkenbusch, K., Probert, P. K., and Hadfield, M. G.: Unusually high food availability in Kaikoura Canyon linked to distinct deep-sea nematode community, Deep Sea Res. Part II Top. Stud. Oceanogr., 104, 310–318, https://doi.org/10.1016/j.dsr2.2013.06.003, 2014.
Leduc, D., Nodder, S. D., Rowden, A. A., Gibbs, M., Berkenbusch, K., Wood, A., De Leo, F., Smith, C., Brown, J., Bury, S. J., and Pallentin, A.: Structure of infaunal communities in New Zealand submarine canyons is linked to origins of sediment organic matter, Limnol. Oceanogr., 104, 1–25, https://doi.org/10.1002/lno.11454, 2020.
Levin, L. A., Etter, R. J., Rex, M. A., Gooday, A. J., Smith, C. R., Pineda, J., Stuart, C. T., Hessler, R. R., and Pawson, D.: Environmental Influences on Regional Deep-Sea Species Diversity, Annu. Rev. Ecol. Syst., 32, 51–93, 2001.
Levin, S. A. and Paine, R. T.: Disturbance, patch formation, and community structure., Proc. Natl. Acad. Sci. USA, 71, 2744–2747, https://doi.org/10.1073/pnas.71.7.2744, 1974.
Liao, J. X., Chen, G. M., Chiou, M. Da, Jan, S., and Wei, C. L.: Internal tides affect benthic community structure in an energetic submarine canyon off SW Taiwan, Deep Sea Res. Part I Oceanogr. Res. Pap. Oceanogra. Res. Pap., 125, 147–160, https://doi.org/10.1016/j.dsr.2017.05.014, 2017.
Lundquist, C. J., Thrush, S. F., Coco, G., and Hewitt, J. E.: Interactions between disturbance and dispersal reduce persistence thresholds in a benthic community, Mar. Ecol. Prog. Ser., 413, 217–228, https://doi.org/10.3354/meps08578, 2010.
Marshall, N. B.: Aspects of Deep Sea Biology, Hutchinson's Scientific and Technical Publications, London, 1954.
Masson, D. G., Kenyon, N. H., and Weaver, P. P. E.: Slides, Debris Flows, and Turbidity Currents, in Oceanography An Illustrated Guide, edited by C. P. Summerhayes and S. A. Thorpe, 136–151, Manson Publishing Ltd., London, 1996.
Maurer, D. O. N., Keck, T., Tinsman, C., and Leathem, W. A.: Vertical Migration adn Mortality of Marine Benthos in Dredged Material: A Synthesis, Int. Rev. ges. Hydrobiol. Hydrogr., 71, 49–63, 1986.
Mayer, L. A., Shor, A. N., Hughes Clarke, J., and Piper, D. J. W.: Dense biological communities at 3850 m on the Laurentian Fan and their relationship to the deposits of the 1929 Grand Banks earthquake, Deep Sea Res. Part I Oceanogr. Res. Pap., 35, 1234–1246, 1988.
Meiburg, E. and Kneller, B.: Turbidity Currents and Their Deposits, Annu. Rev. Fluid Mech., 42, 135–156, https://doi.org/10.1146/annurev-fluid-121108-145618, 2010.
Miller, D. C., Muir, C. L., and Hauser, O. A.: Detrimental effects of sedimentation on marine benthos: What can be learned from natural processes and rates?, Ecol. Eng., 19, 211–232, https://doi.org/10.1016/S0925-8574(02)00081-2, 2002.
Mountjoy, J. J., Howarth, J. D., Orpin, A. R., Barnes, P. M., Bowden, D. A., Rowden, A. A., Schimel, A. C. G., Holden, C., Horgan, H. J., Nodder, S. D., Patton, J. R., Lamarche, G., Gerstenberger, M., Micallef, A., Pallentin, A., and Kane, T.: Earthquakes drive large-scale submarine canyon development and sediment supply to deep-ocean basins, Sci. Adv., 4, 1–8, https://doi.org/10.1126/sciadv.aar3748, 2018.
Naeem, S. and Wright, J. P.: Disentangling biodiversity effects on ecosystem functioning: Deriving solutions to a seemingly insurmountable problem, Ecol. Lett., 6, 567–579, https://doi.org/10.1046/j.1461-0248.2003.00471.x, 2003.
Nardin, T. R., Hein, F. J., Gorsline, D. S., and Edwards, B. D.: A Review of Mass Movement Processes, Sediment, and Acoustic Characteristics, and Contrasts in Slope and Base-of-Slope Systems Versus Canyon-Fan-Basin Floor Systems, Soc Sediment. Geol. SP, 27, 61–73, 1979.
Nelson, C. H., Kulm, L. D., Carlson, P. R., and Duncan, J. R.: Mazama Ash in the Northeastern Pacific, Science, 161, 47–49, https://doi.org/10.1126/science.161.3836.47, 1968.
Newton, P. P., Lampitt, R. S., Jickells, T. D., King, P., and Boutle, C.: Temporal and spatial variability of biogenic particles fluxes during the JGOFS northeast Atlantic process studies at 47∘ N, 20∘ W, Deep Sea Res. Part I Oceanogr. Res. Pap., 41, 1617–1642, https://doi.org/10.1016/0967-0637(94)90065-5, 1994.
Nichols, J. A., Rowe, G. T., Hovey Clifford, C., and Young, R. A.: In Situ Experiments on the Burial of Marine Invertebrates, SEPM J. Sediment. Res., 48, 419–425, https://doi.org/10.1306/212f749b-2b24-11d7-8648000102c1865d, 1978.
Nomaki, H., Mochizuki, T., Kitahashi, T., Nunoura, T., Arai, K., Toyofuku, T., Tanaka, G., Shigeno, S., Tasumi, E., Fujikura, K., and Watanabe, S.: Effects of mass sedimentation events after the 2011 off the Pacific coast of Tohoku Earthquake on benthic prokaryotes and meiofauna inhabiting the upper bathyal sediments, J. Oceanogr., 72, 113–128, https://doi.org/10.1007/s10872-015-0293-5, 2016.
Oguri, K., Kawamura, K., Sakaguchi, A., Toyofuku, T., Kasaya, T., Murayama, M., Fujikura, K., Glud, R. N., and Kitazato, H.: Hadal disturbance in the Japan Trench induced by the 2011 Tohoku-Oki earthquake, Sci. Rep., 3, 1–6, https://doi.org/10.1038/srep01915, 2013.
Oguri, K., Furushima, Y., Toyofuku, T., Kasaya, T., Wakita, M., Watanabe, S., Fujikura, K., and Kitazato, H.: Long-term monitoring of bottom environments of the continental slope off Otsuchi Bay, northeastern Japan, J. Oceanogr., 72, 151–166, https://doi.org/10.10007/s10872-015-0330-4, 2016.
Okey, T. A.: Sediment flushing observations, earthquake slumping, and benthic community changes in Monterey Canyon head, Cont. Shelf Res., 17, 877–897, https://doi.org/10.1016/S0278-4343(96)00067-2, 1997.
Oliver, T. H., Heard, M. S., Isaac, N. J. B., Roy, D. B., Procter, D., Eigenbrod, F., Freckleton, R., Hector, A., Orme, C. D. L., Petchey, O. L., Proença, V., Raffaelli, D., Suttle, K. B., Mace, G. M., Martín-López, B., Woodcock, B. A., and Bullock, J. M.: Biodiversity and Resilience of Ecosystem Functions, Trends Ecol. Evol., 30, 673–684, https://doi.org/10.1016/j.tree.2015.08.009, 2015.
Olu, K., Decker, C., Pastor, L., Caprais, J. C., Khripounoff, A., Morineaux, M., Ain Baziz, M., Menot, L., and Rabouille, C.: Cold-seep-like macrofaunal communities in organic- and sulfide-rich sediments of the Congo deep-sea fan, Deep Sea Res. Part II Top. Stud. Oceanogr., 142, 180–196, https://doi.org/10.1016/j.dsr2.2017.05.005, 2017.
Paine, R. T.: Disaster, Catastrophe, and Local Persistence of the Sea Palm Postelsia palmaeformis, Science, 205, 685–687, https://doi.org/10.1126/science.205.4407.685, 1979.
Paterson, G. L. J. and Lambshead, P. J. D.: Bathymetric patterns of polychaete diversity in the Rockall Trough, northeast Atlantic, Deep Sea Res. Part I Oceanogr. Res. Pap., 42, 1199–1214, https://doi.org/10.1016/0967-0637(95)00041-4, 1995.
Paull, C. K., Schlining, B., Ussler III, W., Lundsten, E., Barry, J. P., Carress, D. W., Johnson, J. E., and McGann, M.: Submarine Mass Transport Within Monterey Canyon: Benthic Disturbance Controls on the Distribution of Chemosynthetic Biological Communities, Springer, Dordrecht, 2010.
Pearcy, W. G., Stein, D. L., and Carney, R. S.: The Deep-Sea Benthic Fish Fauna of the Northeastern Pacific Ocean on Cascadia and Tufts Abyssal Plains and Adjoining Continental Slopes, Biol. Oceanogr., 1, 375–428, https://doi.org/10.1080/01965581.1982.10749448, 1982.
Pickett, S. T. A. and White, P. S.: The Ecology of Natural Disturbance and Patch Dynamics, Elsevier., Academic Press, New York, 1985.
Preen, A. R.: Infaunal Mining: A Novel Foraging Method of Loggerhead Turtles, J. Herpetol., 30, 94, https://doi.org/10.2307/1564718, 1996.
Pruski, A. M., Decker, C., Stetten, E., Vétion, G., Martinez, P., Charlier, K., Senyarich, C., and Olu, K.: Energy transfer in the Congo deep-sea fan: From terrestrially-derived organic matter to chemosynthetic food webs, Deep Sea Res. Part II Top. Stud. Oceanogr., 142, 197–218, https://doi.org/10.1016/j.dsr2.2017.05.011, 2017.
Rathburn, A. E., Levin, L. A., Tryon, M., Gieskes, J. M., Martin, J. B., Pérez, M. E., Fodrie, F. J., Neira, C., Fryer, G. J., Mendoza, G., McMillan, P. A., Kluesner, J., Adamic, J., and Ziebis, W.: Geological and biological heterogeneity of the Aleutian margin (1965–4822 m), Prog. Oceanogr., 80, 22–50, https://doi.org/10.1016/j.pocean.2008.12.002, 2009.
Raup, H. M.: Vegetational adjustment to the instability of the site, 6th Proc. Tech. Meet. Int. Union Conserv. Nat. Nat. Resour, June 1956, Edinburgh, 36–48, 1957.
Reidenauer, J. A. and Thistle, D.: Response of a soft-bottom harpacticoid community to stingray (Dasyatis sabina) disturbance, Mar. Biol., 65, 261–267, https://doi.org/10.1007/BF00397120, 1981.
Richardson, M. D. and Young, D. K.: Abyssal benthos of the Venezuela Basin, Caribbean Sea: standing stock considerations, Deep Sea Res. Part I Oceanogr. Res. Pap., 34, 145–164, https://doi.org/10.1016/0198-0149(87)90079-3, 1987.
Richardson, M. D., Briggs, K. B., and Young, D. K.: Effects of biological activity by abyssal benthic macroinvertebrates on a sedimentary structure in the Venezuela Basin, Mar. Geol., 68, 243–267, https://doi.org/10.1016/0025-3227(85)90015-5, 1985.
Savoye, B., Cochonat, P., Apprioual, R., Bain, O., Baltzer, A., Bellec, V., Beuzart, P., Bourillet, J. F., Cagna, R., Cremer, M., Crusson, A., Dennielou, B., Diebler, D., Droz, L., Ennes, J. C., Floch, G., Guiomar, M., Harmegnies, F., Kerbrat, R., Klein, B., Kuhn, H., Landuré, J. Y., Lasnier, C., Le Drezen, E., Le Formal, J. P., Lopez, M., Loubrieu, B., Marsset, T., Migeon, S., Normand, A., Nouzé, H., Ondréas, H., Pelleau, P., Saget, P., Séranne, M., Sibuet, J. C., Tofani, R., and Voisset, M.: Structure et evolution recente de l'eventail turbiditique du Zaire: Premiers resultats scientifiques des missions d'exploration Zaiango 1 and 2 (marge Congo-Angola), CR. Acad. Sci. II A, 331, 211–220, https://doi.org/10.1016/S1251-8050(00)01385-9, 2000.
Savoye, B., Babonneau, N., Dennielou, B., and Bez, M.: Geological overview of the Angola-Congo margin, the Congo deep-sea fan and its submarine valleys, Deep Sea Res. Part II Top. Stud. Oceanogr., 56, 2169–2182, https://doi.org/10.1016/j.dsr2.2009.04.001, 2009.
Sen, A., Dennielou, B., Tourolle, J., Arnaubec, A., Rabouille, C., and Olu, K.: Fauna and habitat types driven by turbidity currents in the lobe complex of the Congo deep-sea fan, Deep Sea Res. Part II Top. Stud. Oceanogr., 142, 167–179, https://doi.org/10.1016/j.dsr2.2017.05.009, 2017.
Shirayama, Y. and Kojima, S.: Abundance of deep-sea meiobenthos off Sanriku, Northeastern Japan, J. Oceanogr., 50, 109–117, https://doi.org/10.1007/BF02233860, 1994.
Sholkovitz, E. and Soutar, A.: Changes in the composition of the bottom water of the Santa Barbara Basin: effect of turbidity currents, Deep Sea Res. Oceanogr. Abstr., 22, 13–21, https://doi.org/10.1016/0011-7471(75)90014-5, 1975.
Sibuet, M. and Olu, K.: Biogeography, biodiversity and fluid dependence of deep-sea cold-seep communities at active and passive margins, Deep-Sea Res. Pt. I, 45, 517–567, 1998.
Smith, C. R.: Factors Controlling Bioturbation in Deep-Sea Sediments and Their Relation to Models of Carbon Diagenesis, in Deep-Sea Food Chains and the Global Carbon Cycle, pp. 375–393, Springer, the Netherlands, Dordrecht, 1992.
Solheim, A., Bryn, P., Sejrup, H. P., Mienert, J. and Berg, K.: Ormen Lange - An integrated study for the safe development of a deep-water gas field within the Storegga Slide Complex, NE Atlantic continental margin; executive summary, Mar. Pet. Geol., 22, 1–9, https://doi.org/10.1016/j.marpetgeo.2004.10.001, 2005.
Sousa, W. P.: Disturbance in Marine Intertidal Boulder Fields: The Nonequilibrium Maintenance of Species Diversity, Ecology, 60, 1225, https://doi.org/10.2307/1936969, 1979.
Sousa, W. P.: The Role of Disturbance in Natural Communities, Annu. Rev. Ecol. Syst., 15, 353–391, https://doi.org/10.1146/annurev.es.15.110184.002033, 1984.
Sousa, W. P.: Natural Disturbance and the Dynamics of Marine Benthic Communities, in Marine Community Ecology, edited by M. D. Bertness, S. D. Gaines, and M. E. Hay, pp. 85–130, Sinauer Associates, Inc., Sunderland, Massachusetts, 2001.
Stetten, E., Baudin, F., Reyss, J. L., Martinez, P., Charlier, K., Schnyder, J., Rabouille, C., Dennielou, B., Coston-Guarini, J., and Pruski, A.: Organic matter characterization and distribution in sediments of the terminal lobes of the Congo deep-sea fan: Evidence for the direct influence of the Congo River, Mar. Geol., 369, 182–195, https://doi.org/10.1016/j.margeo.2015.08.020, 2015.
Stordal, M. C., Johnson, J. W., Guinasso, N. L., and Schink, D. R.: Quantitative evaluation of bioturbation rates in deep ocean sediments. II. Comparison of rates determined by 210Pb and 239,240Pu, Mar. Chem., 17, 99–114, https://doi.org/10.1016/0304-4203(85)90067-2, 1985.
Talling, P., Clare, M., Urlaub, M., Pope, E., Hunt, J., and Watt, S.: Large Submarine Landslides on Continental Slopes: Geohazards, Methane Release, and Climate Change, Oceanography, 27, 32–45, https://doi.org/10.5670/oceanog.2014.38, 2014.
Talling, P. J.: On the triggers, resulting flow types and frequencies of subaqueous sediment density flows in different settings, Mar. Geol., 352, 155–182, https://doi.org/10.1016/j.margeo.2014.02.006, 2014.
Talling, P. J., Paull, C. K., and Piper, D. J. W.: How are subaqueous sediment density flows triggered, what is their internal structure and how does it evolve? Direct observations from monitoring of active flows, Earth-Sci. Rev., 125, 244–287, https://doi.org/10.1016/j.earscirev.2013.07.005, 2013.
Thomson, J. and Weaver, P. P. E.: An AMS radiocarbon method to determine the emplacement time of recent deep-sea turbidites, Sediment. Geol., 89, 1–7, https://doi.org/10.1016/0037-0738(94)90079-5, 1994.
Thrush, S. F., Pridmore, R. D., Hewitt, J. E., and Cummings, V. J.: Impact of ray feeding disturbances on sandflat macrobenthos: do communities dominated by polychaetes or shellfish respond differently?, Mar. Ecol. Prog. Ser., 69, 245–252, https://doi.org/10.3354/meps069245, 1991.
Thrush, S. F., Hewitt, J. E., Cummings, V. J., Dayton, P. K., Cryer, M., Turner, S. J., Funnell, G. A., Budd, R. G., Milburn, C. J., and Wilkinson, M. R.: Disturbance of the marine benthic habitat by commercial fishing: Impacts at the scale of the fishery, Ecol. Appl., 8, 866–879, https://doi.org/10.1890/1051-0761(1998)008[0866:DOTMBH]2.0.CO;2, 1998.
Thunell, R., Tappa, E., Varala, R., Llano, M., Astor, Y., Muller-Karger, F., and Bohrer, R.: Increased marine sediment suspension and fluxes following an earthquake, Nature, 398, 233–234, https://doi.org/10.1038/18430, 1999.
Thurston, M. H., Bett, B. J., Rice, A. L., and Jackson, P. A. B.: Variations in the invertebrate abyssal megafauna in the North Atlantic Ocean, Deep Sea Res. Part I Oceanogr. Res. Pap., 41, 1321–1348, https://doi.org/10.1016/0967-0637(94)90100-7, 1994.
Thurston, M. H., Rice, A. L., and Bett, B. J.: Latitudinal variation in invertebrate megafaunal abundance and biomass in the North Atlantic Ocean Abyss, Deep Sea Res. Part II Top. Stud. Oceanogr., 45, 203–224, https://doi.org/10.1016/S0967-0645(97)00077-5, 1998.
Tiano, J. C., van der Reijden, K. J., O'Flynn, S., Beauchard, O., van der Ree, S., van der Wees, J., Ysebaert, T., and Soetaert, K.: Experimental bottom trawling finds resilience in large-bodied infauna but vulnerability for epifauna and juveniles in the Frisian Front, Mar. Environ. Res., 159, 104964, https://doi.org/10.1016/j.marenvres.2020.104964, 2020.
Tietjen, J. H.: Distribution and species diversity of deep-sea nematodes in the Venezuela Basin, Deep Sea Res. Part I Oceanogr. Res. Pap., 31, 119–132, https://doi.org/10.1016/0198-0149(84)90019-0, 1984.
Trauthl, M. H., Sarnthein, M., and Arnold, M.: Bioturbational mixing depth and carbon flux at the seafloor, Paleoceanography, 12, 517–526, https://doi.org/10.1029/97PA00722, 1997.
Treignier, C., Derenne, S., and Saliot, A.: Terrestrial and marine n-alcohol inputs and degradation processes relating to a sudden turbidity current in the Zaire canyon, Org. Geochem., 37, 1170–1184, https://doi.org/10.1016/j.orggeochem.2006.03.010, 2006.
Tsujimoto, A., Nomura, R., Arai, K., Nomaki, H., Inoue, M., and Fujikura, K.: Changes in deep-sea benthic foraminiferal fauna caused by turbidites deposited after the 2011 Tohoku-oki earthquake, Mar. Geol., 419, 106045, https://doi.org/10.1016/j.margeo.2019.106045, 2020.
Van Gaever, S., Galéron, J., Sibuet, M., and Vanreusel, A.: Deep-sea habitat heterogeneity influence on meiofaunal communities in the Gulf of Guinea, Deep Sea Res. Part II Top. Stud. Oceanogr., 56, 2259–2269, https://doi.org/10.1016/j.dsr2.2009.04.008, 2009.
Vangriesheim, A., Khripounoff, A., and Crassous, P.: Turbidity events observed in situ along the Congo submarine channel, Deep Sea Res. Part II Top. Stud. Oceanogr., 56, 2208–2222, https://doi.org/10.1016/j.dsr2.2009.04.004, 2009.
Walker, B., Holling, C. S., Carpenter, S. R., and Kinzig, A.: Resilience, adaptability and transformability in social-ecological systems, Ecol. Soc., 9, 1–9, https://doi.org/10.5751/ES-00650-090205, 2004.
Weaver, H.: Fire as an ecological factor in the Southwestern Ponderosa Pine Forests, J. Forest, 49, 93–98, https://doi.org/10.1093/jof/49.2.93, 1951.
Weaver, P. P. E. and Rothwell, R. G.: Sedimentation on the Madeira Abyssal Plain over the last 300 000 years, Geol. Soc. London, Spec. Publ., 31, 71–86, https://doi.org/10.1144/GSL.SP.1987.031.01.07, 1987.
Webb, L. J.: Cyclones as an ecological factor in tropical lowland rain-forest, north queensland, Aust. J. Bot., 6, 220–228, https://doi.org/10.1071/BT9580220, 1958.
Willig, M. R. and Walker, L. R.: Disturbance in terrestrial ecosystems: salient themes, synthesis, and future directions, in: Ecosystems of the World, Elsevier, Amsterdam, 747–768, 1999.
Woods, D. R. and Tietjen, J. H.: Horizontal and vertical distribution of meiofauna in the Venezuela Basin, Mar. Geol., 68, 233–241, https://doi.org/10.1016/0025-3227(85)90014-3, 1985.
Yamanaka, Y. and Kikuchi, M.: Asperity map along the subduction zone in northeastern Japan inferred from regional seismic data, J. Geophys. Res.-Solid Earth, 109, 191–205, https://doi.org/10.1029/2003JB002683, 2004.
Young, D. K. and Richardson, M. D.: Effects of waste disposal on benthic faunal succession on the abyssal seafloor, J. Mar. Syst., 14, 319–336, https://doi.org/10.1016/S0924-7963(97)00033-X, 1998.
Young, D. K., Richardson, M. D., and Briggs, K. B.: Turbidites and benthic faunal succession in the deep sea: an ecological paradox?, https://apps.dtic.mil/sti/citations/ADA403433, 2001.
Turbidity flows – underwater avalanches – are large-scale physical disturbances believed to have profound impacts on productivity and diversity of benthic communities in the deep sea. We reviewed published studies and found that current evidence for changes in productivity is ambiguous at best, but the influence on regional and local diversity is clearer. We suggest study design criteria that may lead to a better understanding of large-scale disturbance effects on deep-sea benthos.
Turbidity flows – underwater avalanches – are large-scale physical disturbances believed to have...