Nematode abundance at the oxygen minimum zone in the Arabian Sea.

By A. Cook, P. Lambshead, L. Hawkins, N. Mitchell, L. Levin. 2000

117 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

ENVIRONMENTAL INFLUENCES ON REGIONAL DEEP-SEA SPECIES DIVERSITY (2001, background): “…groups have been compared, larger taxa (megafauna and macrofauna) exhibit density reductions within the most hypoxic portions of OMZs (Wishner et al. 1990, Levin et al. 1991, 2000) that are not evident in bacteria and metazoan meiofauna (Levin et al. 1991, Cook et al. 2000, Neira et al. in press).”
Is the meiofauna a good indicator for climate change and anthropogenic impacts? (2015, background): “This may explain why in the South Pacific, the relationship between diversity and ecosystem functioning appears weaker, whereas in other regions, such as the Atlantic Ocean and Mediterranean Sea, the relationship is stronger (Leduc et al. 2013).”
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).”
Foraminifera in the Arabian Sea oxygen minimum zone and other oxygen-deficient settings: taxonomic composition, diversity, and relation to metazoan faunas (2000, background): “In general, meiofauna are more tolerant than macrofauna (Josefson and Widbom, 1988; Luth and Luth, 1997) and nematodes are more tolerant than other meiofaunal taxa (Wishner et al., 1990; Levin et al., 1991b; Giere, 1993; Moodley et al., 1997; Cook et al., 2000).”
Effects of natural and human-induced hypoxia on coastal benthos (2009, background): “Among the metazoan meiofauna, nematodes, the numerically dominant and least motile meiofaunal taxon in subtidal soft sediment communities, are the most tolerant to low oxygen (Giere, 1993; Cook et al., 2000; Neira et al., 2001a).”
Meiofaunal distributions on the Peru margin:: relationship to oxygen and organic matter availability (2001, background): “In the present paper, nematode densities were similar to those reported by Cook et al. (2000) for the bathyal Oman margin (range: 494–2495 ind. 10 cm 2).”
Marine nematode deep‐sea biodiversity – hyperdiverse or hype? (2003, background): “This is most clearly seen in marine sediments where abundance declines with depth and distance from the continents (Cook et al., 2000).”
Oxygen minimum zone Benthos: Adaptation and community response to hypoxia (2003, background): “1991a) and with food quality off Oman (hydrogen index; Cook et al. 2000) and Peru (chloroplastic pigment equivalents and labile organic compounds; Neira et al.”
Responses of intertidal nematodes to short-term anoxic events (2007, result): “This confirms that nematodes as a taxon may tolerate oxygen deficiency, although their densities are impaired, as previously reported in field surveys across several habitats as well as in experimental work (e.g. Murell and Fleeger, 1989; Hendelberg and Jensen, 1993; Moodley et al., 1997; Cook et al”
α-, β-, γ-, δ- and ε-diversity of deep-sea nematodes in canyons and open slopes of Northeast Atlantic and Mediterranean margins. (2009, background): “Nematodes are the most abundant metazoan meiofaunal taxon, and their dominance increases with water depth (up to >90%; Thiel 1975, Heip et al. 1985, Cook et al. 2000, Lambshead & Schalk 2001, Danovaro et al. 2002).”
Latitudinal diversity gradients in the deep sea with special reference to North Atlantic nematodes (2000, background): “Polychaetes also show a close association with organic flux compared to molluscs (see Cook et al. 1999) and if these conclusions are correct we predict that polychaete dversity should show similar patterns to nematode diversity.”
Benthic processes on the Peru margin: a transect across the oxygen minimum zone during the 1997–98 El Niño (2002, methodology): “Based on previous studies examining infauna in oxygen minimum zones (Levin et al., 1991, 2000; Levin & Gage, 1998; Cook et al., 2000; Gooday et al., 2000; Gutiérrez et al., 2000; Neira et al., 2001a, b), we hypothesized that oxygen would mainly influence macrofaunal communities and bioturbation,…”