Oceanic primary productivity and dissolved oxygen levels at the Cretaceous/Tertiary Boundary: Their decrease, subsequent warming, and recovery-Reference-Cited by-同舟云学术

Oceanic primary productivity and dissolved oxygen levels at the Cretaceous/Tertiary Boundary: Their decrease, subsequent warming, and recovery

Published:1999-08 Issue:4 Volume:14 Page:511-524
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Kaiho Kunio,Kajiwara Yoshimichi,Tazaki Kazue,Ueshima Masato,Takeda Nobuyori,Kawahata Hodaka,Arinobu Tetsuya,Ishiwatari Ryoshi,Hirai Akio,Lamolda Marcos A.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/v014/i004/1999PA900022/1999PA900022.pdf

Reference65 articles.

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4. Geochemistry of some K/T sections in India;Bhandari;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1993

5. Oxygenand carbon-isotope variations and planktonicforaminifer depth habitats, Late Cretaceous to Paleocene, Central Pacific, Deep Sea Drilling Project sites 463 and 465;Boersma;Initial Rep. Deep Sea Drill. Proj.,1981

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