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David H. Case

Researcher at California Institute of Technology

Publications -  16
Citations -  645

David H. Case is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Anaerobic oxidation of methane & Carbon cycle. The author has an hindex of 11, co-authored 16 publications receiving 541 citations. Previous affiliations of David H. Case include Washington University in St. Louis & Woods Hole Oceanographic Institution.

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Interlaboratory study for coral Sr/Ca and other element/Ca ratio measurements

TL;DR: In this article, an interlaboratory study of coral Sr/Ca measurements was conducted and the results showed that the bias can be significant, and in the extreme case could result in a range in SST estimates of 7°C.
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Environmental and biological controls on Mg and Li in deep-sea scleractinian corals

TL;DR: In this paper, the authors examined the environmental controls on the Mg/Li ratio of 34 individuals from seven genera of deep-sea scleractinian corals: Desmophyllum, Balanophyllia, Caryophyllias, Enallopsammia, Flabellum, Trochocyanthus, and Lophelia.
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Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex

TL;DR: These findings indicate that subduction-associated fluid migration has stimulated microbial activity in the mud reservoir and that mud volcanoes may contribute more substantially to the methane budget than previously estimated.
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Methane Seep Carbonates Host Distinct, Diverse, and Dynamic Microbial Assemblages

TL;DR: In this article, a massively parallel 16S rRNA gene sequencing and statistical analysis was performed on 134 native and experimental samples across 5,500 km, representing a range of habitat substrates (carbonate nodules and slabs, sediment, bottom water and wood) and seepage conditions (active and low activity).
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Microbial abundance and diversity patterns associated with sediments and carbonates from the methane seep environments of Hydrate Ridge, OR

TL;DR: Statistical treatments of relative taxa abundances indicate that archaeal community structure is more dependent on the degree of methane seepage than physical substrate type; bacterial assemblages appear to be more strongly influenced by the type of colonization substrate than seepages activity.