The role of the oceanic oxygen minima in generating biodiversity in the deep sea

By Alex Rogers. 2000

168 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/6c6a77beb7586e0a868f3472bedfbee4b1d0852a

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Citations in the corpus

The exploration of marine biodiversity: scientific and technological challenges (2006, background): “OMZs are formed in areas of high primary production in the surface waters of the ocean and poor water circulation, where the biological degradation of the sinking organic matter results in oxygen depletion (Rogers 2000; Levin 2003).”
Evolutionary pathways among shallow and deep-sea echinoids of the genus Sterechinus in the Southern Ocean (2011, background): “Based on the similarity between the marine benthic fauna of the Antarctic continental shelf and that of the surrounding deep areas, many authors have proposed a continuity of the benthic fauna by means of the abyss, which would allow a connection with the Subantarctic and Magellan zones (Clarke and ”
Evolution and Geological Significance of Larger Benthic Foraminifera (2018, result): “the converging trends highlighted so clearly by Conway Morris (2003). These convergent trends are consistent with developing similar characteristics at different times and probably under similar conditions.”
Deep, diverse and definitely different: unique attributes of the world's largest ecosystem (2010, background): “…mechanisms maintain such high diversity (Grassle and Sanders, 1973; Grassle, 1989; Gage and Tyler, 1991; Etter and Grassle, 1992; Lambshead, 1993; Rogers, 2000; Levin et al., 2001; Snelgrove and Smith, 2002; Rex et al., 2005b) have been constantly discussed and remain controversial (May, 1994).”
The deep-sea floor ecosystem: current status and prospects of anthropogenic change by the year 2025 (2003, background): “…extinctions of deep-sea benthic taxa at the end of the Palaeocene epoch, 65–55 million years ago (mya) associated with a rise in bottom temperature (Rogers 2000), one possible cause being a change or cessation of global thermohaline circulation causing widespread anoxia in deep-ocean bottom…”
Latitudinal diversity patterns of deep-sea marine nematodes and organic fluxes: a test from the central equatorial Pacific (2002, background): “Two characteristics make nematodes different from other taxa, their relatively low ability to disperse (Lambshead 1993) and their resistance to low oxygen conditions (Cook et al. 2000, Rogers 2000, Wetzel et al. 2001).”
Polychaete species diversity in the central Pacific abyss: Local and regional patterns and relationships with productivity (2002, unknown): “…in sediment grain-size diver- sity (Etter & Grassle 1992), large-scale habitat mosaics resulting from submarine canyons and turbidity flows (Levin et al. 2001), variable current regimes, historical contingencies (Etter et al. 1999, Rogers 2000) and latitudinal effects (Rex et al. 1993, 1997, 2000).”
ENVIRONMENTAL INFLUENCES ON REGIONAL DEEP-SEA SPECIES DIVERSITY (2001, background): “During the Late Cretaceous, anoxia sometimes occurred on a much larger scale than in modern oceans, and caused widespread benthic mortality (Rogers 2000).”