Global latitudinal species diversity gradient in deep-sea benthic foraminifera

By S. Culver, M. Buzas. 2000

114 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/5c2f62e49e8d570e6ad24e5acea6f784352b05b9

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Citations in the corpus

Latitudinal diversity patterns of deep-sea marine nematodes and organic fluxes: a test from the central equatorial Pacific (2002, methodology): “Nematodes appear to have a different latitudinal pattern from molluscs, isopods and foraminifers (Rex et al. 1993, 1997, 2000, Culver & Buzas 2000), but possibly have a pattern similar to that of polychaetes (Glover et al. 2001).”
On the Generality of the Latitudinal Diversity Gradient (2004, result): “This does not contradict the ﬁndings that gradients on the two hemispheres differ within single organism groups, among others described for New World birds (Gaston and Williams 1996) and for foraminiferans (Culver and Buzas 2000).”
ENVIRONMENTAL INFLUENCES ON REGIONAL DEEP-SEA SPECIES DIVERSITY (2001, background): “…establishment of a Southern Hemisphere latitudinal gradient in foraminiferan diversity in the late Eocene around 38 my ago, which persists today (Culver & Buzas 1998, 2000), was created by an increase in the seasonally pulsed organic flux that accompanied high latitude, Southern Hemisphere…”
On some hypotheses of diversity of animal life at great depths on the sea floor (2015, background): “For example, for most groups including isopods, gastropods, bivalves, forams, cumaceans (Rex et al. 1993, 1997; Culver & Buzas 2000; Rex et al. 2000; Gage et al. 2004), diversity decreases with increasing latitude in the North Atlantic.”
Introduction to ANDEEP(ANtarctic benthic DEEP -sea biodiversity: colonization history and recent community patterns)—a tribute to Howard L. Sanders (2004, background): “…evidence for the existence of patterns in biodiversity at larger (global) scales; in particular, an apparent decrease in species richness among a number of taxa from the equator towards the poles (Poore and Wilson, 1993; Rex et al., 1993; Thomas and Gooday, 1996; Rex, 1997; Culver and Buzas, 2000).”
Strength, slope and variability of marine latitudinal gradients (2004, background): “Several authors suggested that latitudinal patterns should be different between hemispheres, both for land-living organisms (Blackburn & Gaston 1996, Gaston & Williams 1996) and in the sea (Culver & Buzas 2000, Gray 2001a,b, 2002).”
Patterns, processes and vulnerability of Southern Ocean benthos: a decadal leap in knowledge and understanding (2013, background): “…tendency to gigantism and slow growth; Barnes and Clarke 2011), some significantly (e.g., hemispheric asymmetry in latitudinal diversity gradients; Culver and Buzas 2000; Linse et al. 2006; Clarke et al. 2007) and others have just started to shift (e.g., with regard to ‘large’ geographic range…”
Deep, diverse and definitely different: unique attributes of the world's largest ecosystem (2010, background): “, 1993, 1997, 2000), modern and fossil foraminifera (Thomas and Gooday, 1996; Culver and Buzas, 2000) and nematodes (Lambshead et al.”