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  • PANGAEA  (4)
  • Annual Reviews  (2)
Collection
Keywords
Years
  • 1
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Ecology, Evolution, and Systematics 32 (2001), S. 51-93 
    ISSN: 0066-4162
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Biology
    Notes: Abstract Most of our knowledge of biodiversity and its causes in the deep-sea benthos derives from regional-scale sampling studies of the macrofauna. Improved sampling methods and the expansion of investigations into a wide variety of habitats have revolutionized our understanding of the deep sea. Local species diversity shows clear geographic variation on spatial scales of 100-1000 km. Recent sampling programs have revealed unexpected complexity in community structure at the landscape level that is associated with large-scale oceanographic processes and their environmental consequences. We review the relationships between variation in local species diversity and the regional-scale phenomena of boundary constraints, gradients of productivity, sediment heterogeneity, oxygen availability, hydrodynamic regimes, and catastrophic physical disturbance. We present a conceptual model of how these interdependent environmental factors shape regional-scale variation in local diversity. Local communities in the deep sea may be composed of species that exist as metapopulations whose regional distribution depends on a balance among global-scale, landscape-scale, and small-scale dynamics. Environmental gradients may form geographic patterns of diversity by influencing local processes such as predation, resource partitioning, competitive exclusion, and facilitation that determine species coexistence. The measurement of deep-sea species diversity remains a vital issue in comparing geographic patterns and evaluating their potential causes. Recent assessments of diversity using species accumulation curves with randomly pooled samples confirm the often-disputed claim that the deep sea supports higher diversity than the continental shelf. However, more intensive quantitative sampling is required to fully characterize the diversity of deep-sea sediments, the most extensive habitat on Earth. Once considered to be constant, spatially uniform, and isolated, deep-sea sediments are now recognized as a dynamic, richly textured environment that is inextricably linked to the global biosphere. Regional studies of the last two decades provide the empirical background necessary to formulate and test specific hypotheses of causality by controlled sampling designs and experimental approaches.
    Type of Medium: Electronic Resource
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  • 2
  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Hessler, Robert R; Jumars, Peter A (1974): Abyssal community analysis from replicate cores in the central North Pacific. Deep Sea Research and Oceanographic Abstracts, 21(3), 185-209, https://doi.org/10.1016/0011-7471(74)90058-8
    Publication Date: 2023-05-12
    Description: A 0.25 m**2 United States Naval Electronics Laboratory box corer was used to take replicate samples from an oligotrophic bottom under the North Pacific Central Water Mass (~28°N, 155°W). The bottom is a red clay with manganese nodules at a depth of 5500-5800 m. Macrofaunal density ranges from 84 to 160 individuals per m**2 and is therefore much the same as in Northwest Atlantic Gyre waters. Of the macrofaunal taxa, polychaetes dominate (55 %), followed by tanaids (18 %), bivalves (7 %), and isopods (6 %). Meiofaunal taxa were only partially retained by the 297 µm screen used in washing. Even then, they are 1.5-3.9 times as abundant as the macrofaunal taxa, with nematodes being numerically dominant by far. Foraminifera seem to comprise an important portion of the community, but could not be assessed accurately because of the inability to discriminate living and dead tests. Remains of what are probably xenophyophoridans are also very important, but offer the same problem. Faunal diversity is extremely high, with deposit feeders comprising the overwhelming majority. Most species are rare, being encountered only once. The distributions of only three species show any significant deviation from randomness. The polychaete fauna from box cores collected from 90 miles to the north was not significantly different from that of the principal study locality. Concordance appeared at several taxonomic levels, from species through macrofaunal/meiofaunal relationships. As a result, the variation in total animal abundance shows aggregation among cores. We discuss Sokolova's concept of a deep-sea oligotrophic zone dominated by suspension feeders, and reconcile it with our present findings. The high diversity of the fauna combined with the low food level contradict theories that relate diversity directly with productivity.
    Keywords: 7TOW_7; 7TOW07WT,SIO cruise 123; Argo; BC; Box corer; CLIMAXII-H14; CLIMAXII-H15; CLIMAXII-H16; CLIMAXII-H17; CLIMAXII-H18; CLIMAXII-H3; CLIMAXII-H5; CLIMAXII-H6; CLIMAXII-H7; CLIMAXII-H8; H-03; H-05; H-06; H-07; H-08; H-14; H-15; H-16; H-17; H-18; H-29; H-32; North Pacific; Pacific Ocean; SCAN; Thomas Washington
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Hessler, Robert R; Jumars, Peter A (1974): Abyssal community analysis from replicate cores in the central North Pacific. Deep Sea Research and Oceanographic Abstracts, 21(3), 185-209, https://doi.org/10.1016/0011-7471(74)90058-8
    Publication Date: 2023-08-28
    Description: A 0.25 m US Naval Electronics Lab box corer was used to take replicate samples from an oligotrophic bottom under the North Pacific Central Water Mass (approx. 28 degrees N, 155 degrees W). The bottom is a red clay with manganese nodules at a depth of 5500-5800 m. Macrofaunal density ranges from 84 to 160 individuals per m super(2) and is therefore much the same as in Northwest Atlantic Gyre waters. Of the macrofaunal taxa, polychaetes dominate (55 per cent), followed by tanaids (18 per cent), bivalves (7 per cent), and isopods (6 per cent). Meiofaunal taxa were only partially retained by the 297 micrometer screen used in washing. Even then, they are 1.5-3.9 times as abundant as the microfaunal taxa, with nematodes being numerically dominant by far. Foraminifera seem to comprise an important portion of the community, but could not be assessed accurately because of the inability to discriminate living and dead tests. Remains of what are probably xenophyophoridans are also very important, but offer the same problem. Faunal diversity is extremely high, with deposit feeders comprising the overwhelming majority. Most spp are rare, being encountered only once. The distributions of only 3 spp show any significant deviation from randomness. The polychaete fauna from box cores collected from 90 m to the north was not significantly different from that of the principal study locality. Concordance appeared at several taxonomic levels, from spp through microfaunal/ meiofaunal relationships. As a result, the variation in total animal abundance shows aggregation among cores. The authors discuss Sokolova's concept of a deep-sea oligotrophic zone dominated by suspension feeders, and reconcile it with our present findings. The high diversity of the fauna combined with the low food level contradict theories that relate diversity directly with productivity.
    Keywords: Argo; BC; Box corer; CLIMAXII-075G; CLIMAXII-H14; CLIMAXII-H15; CLIMAXII-H16; CLIMAXII-H17; CLIMAXII-H18; CLIMAXII-H19C; CLIMAXII-H3; CLIMAXII-H5; CLIMAXII-H6; CLIMAXII-H7; CLIMAXII-H8; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dry volume; Elevation of event; Event label; GC; Gravity corer; H-03; H-05; H-06; H-07; H-08; H-14; H-15; H-16; H-17; H-18; H-19C; Latitude of event; Longitude of event; Mass; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optional event label; Pacific Ocean; Photo/Video; Position; PV; Quantity of deposit; Sample ID; SCAN; SCAN-75G; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 111 data points
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  • 5
    Publication Date: 2024-04-29
    Keywords: 7TOW_7; 7TOW07WT,SIO cruise 123; Aplacophora; Argo; Ascidiacea; BC; Bivalvia; Box corer; Brachiopoda; Bryozoa; CLIMAXII-H14; CLIMAXII-H15; CLIMAXII-H16; CLIMAXII-H17; CLIMAXII-H18; CLIMAXII-H3; CLIMAXII-H5; CLIMAXII-H6; CLIMAXII-H7; CLIMAXII-H8; Cnidaria; Copepoda; DEPTH, sediment/rock; Echiurida; Elevation of event; Event label; Gastropoda; H-03; H-05; H-06; H-07; H-08; H-14; H-15; H-16; H-17; H-18; H-29; H-32; Holothuroidea; Isopoda; Latitude of event; Longitude of event; Macrofauna indeterminata; North Pacific; Number of species; Oligochaeta; Ophiuroidea; Ostracoda; Pacific Ocean; Polychaeta; Porifera; SCAN; Scaphopoda; Sipunculida; Tanaidacea; Thomas Washington
    Type: Dataset
    Format: text/tab-separated-values, 246 data points
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  • 6
    Publication Date: 2024-04-29
    Keywords: 7TOW_7; 7TOW07WT,SIO cruise 123; Aplacophora; Argo; Ascidiacea; BC; Bivalvia; Box corer; Brachiopoda; Bryozoa; Carbon, organic, total; CLIMAXII-H14; CLIMAXII-H15; CLIMAXII-H16; CLIMAXII-H17; CLIMAXII-H18; CLIMAXII-H3; CLIMAXII-H5; CLIMAXII-H6; CLIMAXII-H7; CLIMAXII-H8; Cnidaria; Copepoda; DEPTH, sediment/rock; Echiurida; Elevation of event; Event label; Fish teeth; Gastropoda; H-03; H-05; H-06; H-07; H-08; H-14; H-15; H-16; H-17; H-18; H-29; H-32; Holothuroidea; Isopoda; Latitude of event; Longitude of event; Macrofauna, abundance; Macrofauna indeterminata; Meiofauna, abundance of metazoa; Nematoda; Nodules; North Pacific; Oligochaeta; Ophiuroidea; Ostracoda; Pacific Ocean; Polychaeta; Porifera; SCAN; Scaphopoda; Sipunculida; Tanaidacea; Thomas Washington; Volume; Wet mass
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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