Ba/Ca ratios in the non-spinose planktic foraminifer Neogloboquadrina dutertrei: Evidence for an organic aggregate microhabitat-Reference-Cited by-同舟云学术

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Ba/Ca ratios in the non-spinose planktic foraminifer Neogloboquadrina dutertrei: Evidence for an organic aggregate microhabitat

Published:2018-09 Issue: Volume:236 Page:361-372
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Fehrenbacher Jennifer S.,Russell Ann D.,Davis Catherine V.,Spero Howard J.,Chu Edward,Hönisch Bärbel

Funder

US National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference56 articles.

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2. Can microscale chemical patches persist in the sea - microelectrode study of marine snow, fecal pellets;Alldredge;Science,1987

3. Trace element proxies for surface ocean conditions: A synthesis of culture calibrations with planktic foraminifera;Allen;Geochim. Cosmochim. Acta,2016

4. The nitrogen isotope biogeochemistry of sinking particles from the margin of the Eastern North Pacific;Altabet;Deep-Sea Res. Part I-Oceanographic Res. Pap.,1999

5. Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate;Anagnostou;Nature,2016

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4. Geochemical Differences Between Alive, Uncrusted and Dead, Crusted Shells of Neogloboquadrina pachyderma: Implications for Paleoreconstruction;Paleoceanography and Paleoclimatology;2023-10

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