Oxygen minimum zone Benthos: Adaptation and community response to hypoxia

By L. Levin. 2003

842 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/d751b5160dbe02a802f4f5126ace6bc760fd0b27

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Citations in the corpus

Effects of natural and human-induced hypoxia on coastal benthos (2009, background): “Such aggregations, observed in crabs, shrimp and ophiuroids on different margins, appear to be a common feature of lower OMZ boundaries (Levin, 2003).”
Depth zonation and bathymetric trends of deep-sea megafaunal scavengers of the Hawaiian Islands (2009, background): “Drazen (2002), however, concluded that the nutritional condition for some scavenging fishes (C. acrolepis, C. armatus, and C. yaquinae) is not affected by seasonality in carbon export to the seafloor off the California coast, where extreme seasonal variations exist in surface production and particle”
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).”
Late Ediacaran redox stability and metazoan evolution (2012, background): “, (Diaz and Rosenberg, 1995; Levin, 2003)).”
Declining oxygen in the global ocean and coastal waters (2018, background): “Low oxygen can reduce survival and growth and alter behavior of individual organisms (3, 4, 26, 64).”
Characteristics of meiofauna in extreme marine ecosystems: a review (2018, background): “…Phleger and Soutar 1973; Perez-Cruz and Machain-Castillo 1990; Sen Gupta and Machain-Castillo 1993; Bernhard and Sen Gupta 1999; Gooday et al. 2000; Levin 2003); (2) the presence of bacterial endosymbionts (e.g. Bernhard 2003); (3) the sequestration of chloroplasts (Bernhard and Bowser 1999;…”
Hypoxia-based habitat compression of tropical pelagic fishes (2006, background): “The subsequent in situ decomposition of organic matter at depth, stagnant deep water layers, the advection process and absence of significant mixing in these areas all contribute to the development of hypoxic environments (Cushing, 1969; Levin, 2003) where low DO concentrations would be physiologica”
The humboldt current system of northern and central chile : Oceanographic processes, ecological interactions and socioeconomic feedback (2007, background): “On the other hand, within the OMZ eukaryotes are in general small-size forms, like meiofauna, calcareous foraminiferans and nematodes (Gooday et al. 2000, Neira et al. 2001, Levin 2003).”
Responses of intertidal nematodes to short-term anoxic events (2007, background): “In addition, nematodes and foraminiferans may reach high abundances in marine Oxygen Minimum Zones (OMZ), where they presumably benefit from the abundant food supply and the release from predation (Neira et al., 2001; Levin, 2003).”
Reviews and syntheses: to the bottom of carbon processing at the seafloor (2017, background): “Moreover, in modern systems with anoxic bottom waters benthic animals are absent (Rhoads and Morse, 1971; Diaz and Rosenberg, 1995, 2008; Levin, 2003; Levin et al., 2009).”
Oxygen as a control on sea floor biological communities and their roles in sedimentary carbon cycling (2007, background): “We predict that in very low-O2 environments and in relatively OM-poor, oxygenated environments, foraminifera will tend to dominate OM uptake and preliminary processing, whereas at selected OM-rich sites with slightly higher O2 concentrations (such as at lower boundaries of OMZs), metazoan macrofauna”
Man and the Last Great Wilderness: Human Impact on the Deep Sea (2011, background): “Faunal assemblages exhibit low density, low diversity, and sometimes small body size [239,259].”
ECOLOGY OF COLD SEEP SEDIMENTS: INTERACTIONS OF FAUNA WITH FLOW, CHEMISTRY AND MICROBES (2005, background): “Seismic documentation of bottom simulating reflectors indicative of hydrates on the Chile margin (Morales 2003) and dredged seep bivalves (Stuardo & Valdovinos 1988, Sellannes et al. 2004) indicate the existence of many more (as yet unlocated) seeps in subduction settings.”
A basin redox transect at the dawn of animal life (2012, background): “…to lie in their very small, thin body plans (with high surface-area to volume ratios for increased diffusion) and enlarged respiratory organs (Levin, 2003; Gooday et al., 2010; Jeffreys et al., 2012; Lamont and Gage, 2000; Neira et al., 2001)—that is, with morphological adaptations that…”
Deep, diverse and definitely different: unique attributes of the world's largest ecosystem (2010, background): “…depths where in situ photosynthesis leads to much greater background levels of productivity, some of these same habitat islands (e.g. vents, seeps, low-oxygen zones) may have yielded relatively few adaptive radiations and little evolutionary novelty (Levin, 2003; Tarasov et al., 2005; Smith, 2006).”
GLOBAL MARINE BIODIVERSITY TRENDS (2006, background): “The benthic communities in the minimum oxygen zone support low-diversity mats of large sulfide-oxidizing bacteria (142).”
Time-series analysis of six whale-fall communities in Monterey Canyon, California, USA (2010, unknown): “Oxygen minimum zones, characterized by 40.5 ml/L of O2 tend to be associated with lower species diversity in the deep sea (Levin and Atkinson, 2003), but it remains unclear whether these trends can be extended to whale-falls implanted in Monterey Canyon (i.e., whales 633 and 1018; Braby et al.,…”