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  • 1
    ISSN: 1573-5117
    Keywords: rocky subtidal community ; long-term ; fluctuations ; recruitment ; predation ; common trends
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Inside the COST 647 Rocky Subtidal Programme, as well as before this came into operation, a cooperation has been developed between Swedish and Norwegian groups working with rocky subtidal ecology in the Skagerrak area. Along a coastline of more than 300 km, and additional large fjord systems, natural fixed-site rocky subtidal communities have been stereophotographically recorded more or less seasonally over a considerable number of years (15 in Sweden and 7 in Norway). Additional experimental studies have been undertaken in situ. Inter-site comparisons revealed many examples of co-variation in long-term population fluctuations. A common 7-year cyclic pattern was clearly illustrated for the ascidian Ciona intestinalis and the echinoid Echinus esculentus. Similar long-term trends were found in populations of Asterias rubens, Ascidia mentula, Sabella penicillus, Crania anomala and Protantea simplex over the time periods available for comparison. Locally deviating populations were also found, however. Major structuring factors, as well as key species, appeared to be largely the same over the geographic range studied. By comparing all of our results (mostly based on already published data), recruitment and predation were found to be the most important locally organizing factors. Recruitment strategies and patterns influenced both community structure and long-term trends. Predation by echinoderms and gastropods modified the structure of established communities. The common key predator in the area, Asterias rubens, largely influenced community structure by selective predation on the dominant competitors Ciona intestinalis and Mytilus edulis which, in the absence of predation, appeared to be highly capable of substrate monopolization in various parts of the studied communities, depending on depth and exposure. The results indicate the existence of large-scale structuring factors, probably linked to climatic events. This is considered as an important pre-requisite for the future recognition and understanding of local deviations, e.g. as results of pollution. This study also pinpoints some species and processes that should be focussed upon in monitoring programs.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-5117
    Keywords: rocky subtidal communities ; algae ; eutrophication ; long-term change ; predation ; Skagerrak
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Rocky subtidal communities on the Swedish west coast were monitored over approximately 16 years (1970–1985) by means of stereophotographic recordings, at intervals, of fixed sites. Dominating elements of community structure were studied at the 5- and 10 m depth levels of an outer archipelago locality. Excluding seasonal variations, the basic community structure, largely dominated by the perennial phaeophycean Halidrys siliquosa (L.), remained relatively stable over the first 7–8 years of study, but with an increasing trend in cover of filamentous epiphytic red algae. Later, the structure of the studied communities changed radically. The changes initially involved intense settling of the blue mussel Mytilus edulis L. and reduced cover of red algae. The mussels settled largely on Halidrys plants which eventually broke down almost completely. Later, there was intensive predation on Mytilus by the starfish Asterias rubens Linné. After the elimination of Mytilus, the studied test areas were dominated by filamentous ephemeral red algae for the rest of the study period, but with some regeneration of Halidrys at the 5 m level. The observed changes were thought to be indicative of a major disturbance in the coastal ecosystems off the Swedish west coast during the studied period. This notion is discussed in relation to studies of other components of the ecosystem during the same time period and in relation to possible causes. Among the latter may be mentioned a suspected eutrophication process, long-term temperature anomalies and resulting effects on biological interrelationships such as competition, predation and chemical defense. The observed trends included a shift in dominance from slow-growing perennial algae to fast-growing ephemeral algae. If this shift was a general phenomenon, for which there is some circumstantial evidence, it could have important repercussions on the cycling of nutrients and organic matter in the coastal ecosystem. Possible effects are discussed on hypothetical terms in relation to observed anomalies in phytoplankton blooms and benthic oxygenation.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2020-07-23
    Description: Cold-watercoralreefs occur in many regions of the world's oceans. Fundamental questions regarding their functioning remain unanswered. These include the biogeochemical influence of reefs on their environment (“reef effects”) and the influence of hydrodynamic processes on reef nutrition. In a succession of field campaigns in 2007 and 2008, these questions were addressed at the Tislercold-watercoralreef, which is centered on a sill peak in the Norwegian Skagerrak. A variety of methodological approaches were used. These consisted of the collection of CTD and chlorophyll profiles, current measurements, sampling of particulateorganicmatter (POM) in the benthic boundary layer (BBL) across the reef with subsequent chemical analyses, and the chemical analysis of freshly released Lophelia pertusa mucus. CTD and chlorophyll profiles indicated that downstream of the sill crest, downwelling delivered warmer, fresher and chlorophyll richer water masses down to the BBL. Both sides of the reef received downwelling nutrition delivery, as flow direction over the reef reversed periodically. Several chemical composition indicators revealed that suspended POM was significantly fresher on the downstream side of the reef than on the upstream side. L. pertusa mucus from the TislerReef was labile in composition, as indicated by a low C/N ratio and a high amino acid degradation index (DI) value. Particulateorganic carbon (POC) content in the BBL was significantly depleted across the reef. Lateral depositional fluxes were calculated to be 18–1485 mg POC m−2 d−1, with a mean of 459 mg POC m−2 d−1. We propose that the combination of fresh, downwelling POM with mucus released from the reef was the cause of the greater lability of the downstream POM. Our data on POC depletion across the reef suggest that cold-watercoralreefs could play an important role in carbon cycling along continental margins. Research Highlights: ► Downwelling is important for reef nutrition of cold-watercoralreefs located on sills. ► Lophelia pertusa mucus is a labile organic substrate. ► POM on the downstream side of a reef can be more labile than on the upstream side. ► POC content in the BBL was significantly depleted across TislerReef. ► Cold-watercoralreefs could play an important role in carbon cycling in the oceans.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 4
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    Springer
    In:  In: Cold-Water Corals and Ecosystems. , ed. by Freiwald, A. and Roberts, J. M. Erlangen Earth Conference Series . Springer, Berlin, pp. 771-805.
    Publication Date: 2017-07-07
    Description: The rate of discovery of reefs of the cold-water coral Lophelia pertusa (Linnaeus, 1758) has been remarkable, and attributable to the increased use of underwater video. These reefs form a major three-dimensional habitat in deeper waters where little other ‘cover’ for fish is available. They are common in the eastern North Atlantic, and occur at least in the western North Atlantic and off central Africa. There are also other non-reef records of Lophelia in the Atlantic, and in Indian and Pacific oceans. Thus, not only are these reefs a significant habitat on a local scale, but they may also provide an important habitat over a very wide geographic scale. The present study examined the association of fish species with Lophelia in the Northeast Atlantic, including the Trondheimsfjord and Sula Ridge in Norway, Kosterfjord in Sweden, Darwin Mounds west of Scotland, and Rockall Bank, Rockall Trough and Porcupine Seabight off Ireland. The fish fauna associated with a shipwreck west of Shetland was also studied. Data were collected from 11 study sites at 8 locations, using 52 hours of video and 15 reels of still photographs. Video and still photographs were collected from (1) manned submersible, (2) surface controlled remotely operated vehicle (ROV), (3) a towed “hopper” camera, (4) wide angle survey photography (WASP), (5) seabed high resolution imaging platform (SHRIMP), and (6) an in situ time-lapse camera “Bathysnap”. It was possible to identify 90 % of fish observed to species level and 6.5 % to genus or family level. Only 3.5 % of the fish were not identifiable. A guide to the fishes is given at http://www.ecoserve.ie/projects/aces/. Twenty-five species of fishes from 17 families were recorded over all the sites, of which 17 were of commercial importance and comprised 82 % of fish individuals observed. These commercial fish species contribute 90 % of commercial fish tonnage in the North Atlantic. The habitats sampled were comprised of 19 % reef, 20 % transitional zone (i.e. between living coral and debris zone), 25 % coral debris and 36 % off-reef seabed. Depth was the most significant parameter in influencing the fish associated with the reefs, both at the species and family level. There was a complete separation of sites above and below 400–600 m depth by multi-dimensional scaling (MDS) analysis. Less distinct assemblages of fish species were associated with each habitat. Fish species richness and abundance was greater on the reef than surrounding seabed. In fact, 92 % of species, and 80 % of individual fish were associated with the reef. The present data indicates that these reefs have a very important functional role in deep-water ecosystems as fish habitat.
    Type: Book chapter , NonPeerReviewed
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  • 5
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    PANGAEA
    In:  Supplement to: Wienberg, Claudia; Titschack, Jürgen; Freiwald, André; Frank, Norbert; Lundälv, Tomas; Taviani, Marco; Beuck, Lydia; Schröder-Ritzrau, Andrea; Krengel, Thomas; Hebbeln, Dierk (2018): The giant Mauritanian cold-water coral mound province: Oxygen control on coral mound formation. Quaternary Science Reviews, 185, 135-152, https://doi.org/10.1016/j.quascirev.2018.02.012
    Publication Date: 2023-09-21
    Description: The largest coherent cold-water coral (CWC) mound province in the Atlantic Ocean exists along the Mauritanian margin, where up to 100 m high mounds extend over a distance of ~400 km, arranged in two slope-parallel chains in 400-550 m water depth. Additionally, CWCs are present in the numerous submarine canyons with isolated coral mounds being developed on some canyon flanks. Seventy-seven Uranium-series coral ages were assessed to elucidate the timing of CWC colonisation and coral mound development along the Mauritanian margin for the last ~120,000 years. Our results show that CWCs were present on the mounds during the Last Interglacial, though in low numbers corresponding to coral mound aggradation rates of 16 cm kyr**-1. Most prolific periods for CWC growth are identified for the last glacial and deglaciation, resulting in enhanced mound aggradation (〉1000 cm kyr**-1), before mound formation stagnated along the entire margin with the onset of the Holocene. Until today, the Mauritanian mounds are in a dormant state with only scarce CWC growth. In the canyons, live CWCs are abundant since the Late Holocene at least. Thus, the canyons may serve as a refuge to CWCs potentially enabling the observed modest re-colonisation pulse on the mounds along the open slope. The timing and rate of the pre-Holocene coral mound aggradation, and the cessation of mound formation varied between the individual mounds, which was likely the consequence of vertical/lateral changes in water mass structure that placed the mounds near or out of oxygen-depleted waters, respectively.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2024-02-02
    Keywords: 1049-1; 1069-2; 1070-2; 1071-2; 965-2; Age, maximum/old; Age, minimum/young; Age, optional; Center for Marine Environmental Sciences; Cluster number; Elevation of event; Event label; GC; GeoB11569-1; GeoB14799-2; GeoB14882-1; GeoB14884-1; GeoB14903-2; GeoB14904-2; GeoB14905-2; Gravity corer; Latitude of event; Location; Longitude of event; Maria S. Merian; MARUM; MSM16/3; MSM16/3_1051-1; northern Banda slide; northern canyon area west of Banc dArguin (ROV3); off Mauritania; POS346; POS-346; POS346_69-1; Poseidon; Sedimentation rate; Timiris shallow coral mound chain
    Type: Dataset
    Format: text/tab-separated-values, 92 data points
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  • 7
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    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-03-01
    Keywords: ANT-XXVII/3; AWI_BPP; Bentho-Pelagic Processes @ AWI; DATE/TIME; Date/time end; Date/time start; File name; File size; Polarstern; PS77; PS77/253-1; Remote operated vehicle Sperre SubFighter 7500 DC; ROVSP; Uniform resource locator/link to movie; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Fillinger, Laura; Janussen, Dorte; Lundälv, Tomas; Richter, Claudio (2013): Rapid Glass Sponge Expansion after Climate-Induced Antarctic Ice Shelf Collapse. Current Biology, 23(14), 1330-1334, https://doi.org/10.1016/j.cub.2013.05.051
    Publication Date: 2024-03-01
    Description: Over 30% of the Antarctic continental shelf is permanently covered by floating ice shelves, providing aphotic conditions for a depauperate fauna sustained by laterally advected food. In much of the remaining Antarctic shallows (〈300 m depth), seasonal sea-ice melting allows a patchy primary production supporting rich megabenthic communities dominated by glass sponges (Porifera, Hexactinellida). The catastrophic collapse of ice shelves due to rapid regional warming along the Antarctic Peninsula in recent decades has exposed over 23,000 km**2 of seafloor to local primary production. The response of the benthos to this unprecedented flux of food is, however, still unknown. In 2007, 12 years after disintegration of the Larsen A ice shelf, a first biological survey interpreted the presence of hexactinellids as remnants of a former under-ice fauna with deep-sea characteristics. Four years later, we revisited the original transect, finding 2- and 3-fold increases in glass sponge biomass and abundance, respectively, after only two favorable growth periods. Our findings, along with other long-term studies, suggest that Antarctic hexactinellids, locked in arrested growth for decades, may undergo boom-and-bust cycles, allowing them to quickly colonize new habitats. The cues triggering growth and reproduction in Antarctic glass sponges remain enigmatic.
    Keywords: AWI_BPP; Bentho-Pelagic Processes @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
    Publication Date: 2024-03-01
    Keywords: ANT-XXVII/3; AWI_BPP; Bentho-Pelagic Processes @ AWI; Event label; File format; File name; File size; Identification; Polarstern; PS77; PS77/264-1; PS77/272-1; PS77/275-4; PS77/278-1; PS77/287-1; PS77/299-1; PS77/306-1; Remote operated vehicle; ROV; Species; Uniform resource locator/link to file; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 892 data points
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  • 10
    Publication Date: 2024-01-19
    Description: Cold-water corals form prominent reef ecosystems along ocean margins that depend on suspended resources produced in surface waters. In this study, we investigated food processing of 13C and 15N labelled bacteria and algae by the cold-water coral Lophelia pertusa. Coral respiration, tissue incorporation of C and N and metabolic-derived C incorporation into the skeleton were traced following the additions of different food concentrations (100, 300, 1300 µg C/l) and two ratios of suspended bacterial and algal biomass (1:1, 3:1). Respiration and tissue incorporation by L. pertusa increased markedly following exposure to higher food concentrations. The net growth efficiency of L. pertusa was low (0.08±0.03), which is consistent with their slow growth rates. The contribution of algae and bacteria to total coral assimilation was proportional to the food mixture in the two lowest food concentrations, but algae were preferred over bacteria as food source at the highest food concentration. Similarly, the stoichiometric uptake of C and N was coupled in the low and medium food treatment, but was uncoupled in the high food treatment and indicated a comparatively higher uptake or retention of bacterial carbon as compared to algal nitrogen. We argue that behavioural responses for these small-sized food particles, such as tentacle behaviour, mucus trapping and physiological processing, are more likely to explain the observed food selectivity as compared to physical-mechanical considerations. A comparison of the experimental food conditions to natural organic carbon concentrations above CWC reefs suggests that L. pertusa is well adapted to exploit temporal pulses of high organic matter concentrations in the bottom water caused by internal waves and down-welling events.
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 47.6 kBytes
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