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. 2009 Dec 14;106(51):21717–21720. doi: 10.1073/pnas.0910935106

Fig. 4.

Fig. 4.

Tropical deep-sea benthic species diversity and climatic and paleoecological factors. Relationships between ODP 925 diversity [E(50)] and (A) deep-sea oxygen isotope (37), (B) bottom-water temperature (BWT) (60), and (C) surface productivity (44). (D) Comparison between relative abundance of slope species and deep-sea oxygen isotope (37).