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  • 2020-2024  (7)
  • 1985-1989
  • 1980-1984
  • 2023  (5)
  • 2020  (2)
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  • 1
    Publication Date: 2024-02-07
    Description: Driven by climate change, marine biodiversity is undergoing a phase of rapid change that has proven to be even faster than changes observed in terrestrial ecosystems. Understanding how these changes in species composition will affect future marine life is crucial for conservation management, especially due to increasing demands for marine natural resources. Here, we analyse predictions of a multiparameter habitat suitability model covering the global projected ranges of 〉33,500 marine species from climate model projections under three CO2 emission scenarios (RCP2.6, RCP4.5, RCP8.5) up to the year 2100. Our results show that the core habitat area will decline for many species, resulting in a net loss of 50% of the core habitat area for almost half of all marine species in 2100 under the high-emission scenario RCP8.5. As an additional consequence of the continuing distributional reorganization of marine life, gaps around the equator will appear for 8% (RCP2.6), 24% (RCP4.5), and 88% (RCP8.5) of marine species with cross-equatorial ranges. For many more species, continuous distributional ranges will be disrupted, thus reducing effective population size. In addition, high invasion rates in higher latitudes and polar regions will lead to substantial changes in the ecosystem and food web structure, particularly regarding the introduction of new predators. Overall, our study highlights that the degree of spatial and structural reorganization of marine life with ensued consequences for ecosystem functionality and conservation efforts will critically depend on the realized greenhouse gas emission pathway.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-05-07
    Description: The PAN-Arctic data collection of benthic BIOtas (PANABIO) contains records of benthic fauna identified at genus-level or species-level in field samples taken at point-referenced locations (stations) by means of grabs, towed gear, or seabed imaging. The data are from all major marine Arctic areas, i.e., central Arctic Ocean, Chukchi Sea, East Siberian Sea, Laptev Sea, Kara Sea, Barents Sea (incl. White Sea), Svalbard waters, Greenland Sea, Norwegian Sea, Canadian Archipelago, Beaufort Sea, and Bering Sea, as well as some adjacent sub-Arctic regions (Sea of Japan, Gulf of Okhotsk). Currently (14 December 2023), the collection includes 27 datasets with a total of 126,388 records (ranging from presence to counts, abundances or biomass) of 2,978 taxa, identified in 11,555 samples taken at 10,596 stations during 1,095 cruises between 1800 and 2014. It is also available in a PostgreSQL-based data warehouse that can be accessed and queried through an open-access frontend web service at https://critterbase.awi.de/panabio.
    Keywords: Arctic; Benthos; Biodiversity; biogeography
    Type: Dataset
    Format: application/zip, 27 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-06-25
    Description: The dataset comprises a total of 9,540 records of semi-quantitative data for 53 benthic invertebrate taxa and fish from 180 trawl samples (Agassiz trawl, bottom trawl, Rauschert dredge, benthopelagic trawl). The semi-quantitative data represent four categories regarding the frequency of occurrence of the benthic taxa (i.e. 0 = absent, 1 = rare, 2 = common and 3 = very common). The dataset was collected on the shelf and slope of the eastern Weddell Sea and Lazarev Sea, near Bouvet Island and the region at the north western tip of the Antarctic Peninsula (depth range: 64 - 2334 m) between 1989 and 2004 onboard "Polarstern". Cruises ANT VII/4 (1989), ANT IX/3 (1990/91), ANT XIII/3 (1996), ANT XV/3 (1998) and ANT XXI/2 (2003/2004) contributed to the data collection.
    Keywords: Acari; Actiniaria; Agassiz Trawl; AGT; Alcyonacea; Amphipoda; ANT-IX/3; ANT-VII/4; ANT-XIII/3; ANT-XV/3; ANT-XXI/2; Aplacophora; Ascidiacea; Asteroidea; Bentho-pelagic trawl; Bivalvia; Bottom trawl; BPT; Brachiopoda; Bryozoa; BT; Campaign; Cephalopoda; Cirripedia; Crinoidea; Cumacea; DATE/TIME; Date/time end; Decapoda; Demospongia; DEPTH, water; Drake Passage; Dredge, Rauschert; Drescher Inlet; Eastern Weddell Sea, Southern Ocean; Echinoidea; Echiurida; Errantia; Event label; Gear; Gorgonariana; Graptolithoidea; Halley Bay; Haul 8; Height; Hexacorallia; Hexactinellida; Holothuroidea; Hydroidolina; Hydrozoa; Isopoda; Kapp Norvegia; King George Island, Antarctic Peninsula; LATITUDE; Lazarev Sea; Leptostraca; LONGITUDE; Mesh size; MULT; Multiple investigations; Mysida; Nematoda; Nemertea; Nudibranchia; Ophiuroidea; Opisthobranchia; Ostracoda; Pantopoda; Pennatula; Pisces; Platyhelminthes; Polarstern; Polyplacophora; Porifera; Priapulida; Project; Prosobranchia; PS14/211; PS14/212; PS14/217; PS14/224; PS14/226; PS14/229; PS14/230; PS14/235; PS14/235-1; PS14/241; PS14/241-1; PS14/245; PS14/245-1; PS14/248; PS14/249; PS14/249-1; PS14/250; PS14/250-1; PS14/252; PS14/253; PS14/256; PS14/257; PS14/258; PS14/259; PS14/260; PS14/261; PS14/269; PS14/270; PS14/271; PS14/272; PS14/273; PS14/274; PS14/275; PS14/281; PS14/282; PS14/284; PS14/289; PS14/290; PS14/291; PS14/293; PS14 EPOS I; PS18; PS18/123-1; PS18/129-1; PS18/130-1; PS18/133-1; PS18/135-2; PS18/158-1; PS18/160-2; PS18/162-1; PS18/165-2; PS18/168-1; PS18/169-1; PS18/171-2; PS18/173-1; PS18/174-1; PS18/176-1; PS18/179-1; PS18/180-3; PS18/189-3; PS18/192-2; PS18/206-1; PS18/207-2; PS18/211-1; PS18/212-8; PS18/220-2; PS39/001-1; PS39/002-9; PS39/004-4; PS39/005-11; PS39/006-12; PS39/006-15; PS39/009-1; PS39/009-15; PS39/009-18; PS39/011-1; PS39/012-1; PS39/013-4; PS39/014-2; PS39/015-1; PS39/016-1; PS39/017-1; PS39/018-1; PS39/024-2; PS39/025-1; PS39/025-13; PS39/029-1; PS39/030-2; PS39 EASIZ; PS48/006; PS48/037; PS48/039; PS48/044; PS48/049; PS48/050; PS48/062; PS48/071; PS48/077; PS48/082; PS48/088; PS48/095; PS48/097; PS48/100; PS48/115; PS48/120; PS48/123; PS48/128; PS48/134; PS48/141; PS48/144; PS48/150; PS48/154; PS48/157; PS48/166; PS48/167; PS48/168; PS48/172; PS48/189; PS48/194; PS48/197; PS48/198; PS48/206; PS48/214; PS48/220; PS48/222; PS48/277; PS48/295; PS48/296; PS48/303; PS48/308; PS48/322; PS48/324; PS48/329; PS48/336; PS48/337; PS48/338; PS48/346; PS48/348; PS48/352; PS48/355; PS48 EASIZ II; PS65/019-1; PS65/020-1; PS65/028-1; PS65/029-1; PS65/039-1; PS65/090-1; PS65/109-1; PS65/121-1; PS65/132-1; PS65/161-1; PS65/173-1; PS65/233-1; PS65/245-1; PS65/248-1; PS65/253-1; PS65/259-1; PS65/265-1; PS65/274-1; PS65/276-1; PS65/278-1; PS65/279-1; PS65/280-1; PS65/292-1; PS65/336-1; PS65/344-1; PS65 BENDEX; Pycnogonida; RD; Sample ID; Scaphopoda; Scleractinia; Sedentaria; Ship speed; Siboglinidae; Sipuncula; South Atlantic Ocean; South of Vestkapp; Station label; Stolonifera; Stylasteridae; Tanaidacea; Trawling time; Turbellaria; Weddell Sea; Width
    Type: Dataset
    Format: text/tab-separated-values, 11229 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-07-06
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 5
    Publication Date: 2023-09-22
    Description: Driven by climate change, marine biodiversity is undergoing a phase of rapid change that has proven to be even faster than changes observed in terrestrial ecosystems. Understanding how these changes in species composition will affect future marine life is crucial for conservation management, especially due to increasing demands for marine natural resources. Here, we analyse predictions of a multiparameter habitat suitability model covering the global projected ranges of 〉33,500 marine species from climate model projections under three CO2 emission scenarios (RCP2.6, RCP4.5, RCP8.5) up to the year 2100. Our results show that the core habitat area will decline for many species, resulting in a net loss of 50% of the core habitat area for almost half of all marine species in 2100 under the high-emission scenario RCP8.5. As an additional consequence of the continuing distributional reorganization of marine life, gaps around the equator will appear for 8% (RCP2.6), 24% (RCP4.5), and 88% (RCP8.5) of marine species with cross-equatorial ranges. For many more species, continuous distributional ranges will be disrupted, thus reducing effective population size. In addition, high invasion rates in higher latitudes and polar regions will lead to substantial changes in the ecosystem and food web structure, particularly regarding the introduction of new predators. Overall, our study highlights that the degree of spatial and structural reorganization of marine life with ensued consequences for ecosystem functionality and conservation efforts will critically depend on the realized greenhouse gas emission pathway.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-01-31
    Description: The authors regret that the specified units of bioirrigation activity (Ic) and the indices (i.e. IPc,AFDM, IPc,WM, BPc,WM, BPc,AFDM) were incorrect in the original publication. Bioirrigation activity was presented in l/m25 min rather than in l/m2h and the indices were calculated per experimental core rather than per m2. Nevertheless, this does not affect the results and also the conclusions remain unchanged. AICc values for the best models of IPc,AFDM, IPc,WM, BPc,WM, BPc,AFDM have not changed in relation to each other, although they differ in value. The corrected version of Appendix B includes the corrected statistical details (i.e. AICc values). The corrected version of the Fig. 1 is provided below. The authors would like to apologize for any inconvenience caused.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 7
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    Elsevier
    In:  EPIC3Journal of Environmental Management, Elsevier, 347, pp. 119022-119022, ISSN: 0301-4797
    Publication Date: 2024-01-31
    Description: At the end of their operational life time offshore wind farms need to be decommissioned. How and to what extent the removal of the underwater structures impairs the ecosystem that developed during the operational phase of the wind farm is not known. So, decision makers face a knowledge gap, making the consideration of such ecological impacts challenging when planning decommissioning. This study evaluates how complete or partial decommissioning of foundation structure and scour protection layer impacts local epibenthic macrofauna biodiversity. We assessed three decommissioning alternatives (one for complete and two for partial removal) regarding their impact on epibenthic macrofauna species richness. The results imply that leaving the scour protection layer in situ will preserve a considerable number of species while cutting of the foundation structure above seabed will be beneficial for the fauna of such foundation structures where no scour protection is installed. These results should be taken with a grain of salt, as the current data base is rather limited. Data need to be improved substantially to allow for reliable statements and sound advice regarding the ecological impact of offshore wind farm decommissioning.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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