Stoll, Heather M. (2004): Coccolith Sr/Ca records of productivity during the Paleocene-Eocene thermal maximum from the Weddell Sea; reply

Leg/Site/Hole:
ODP 113
ODP 113 690
Identifier:
2005-037144
georefid

10.1029/2003PA000971
doi

Creator:
Stoll, Heather M.
Williams College, Department of Geosciences, Williamstown, MA, United States
author

Identification:
Coccolith Sr/Ca records of productivity during the Paleocene-Eocene thermal maximum from the Weddell Sea; reply
2004
Paleoceanography
American Geophysical Union, Washington, DC, United States
19
1
3
Stoll's reply to comments made by Bralower, et. al. Modified abstrct of original article: A major perturbation of the global carbon cycle 55 million years ago, believed to result from release of 1000-2000 Gt of C from methane hydrates, correlates with an intense but transient greenhouse warming event known as the Paleocene Eocene Thermal Maximum (PETM). The rapid (105 years) recovery of global temperatures reflects important negative feedbacks in the climate system and carbon cycle. A new independent indicator, Sr/Ca in coccolith carbonate, which covaries with the productivity of coccolithophorid algae, is used to investigate the biotic response in the most complete PETM deep sea record which was recovered at ODP Site 690 in the Weddell Sea. (modified journ. abstr.)
English
Coverage:Geographic coordinates:
North:-65.0937
West:1.1218East: 1.1218
South:-65.0938

Stratigraphy; algae; alkaline earth metals; biochemistry; calcium; Cenozoic; Coccolithophoraceae; Eocene; Leg 113; marine environment; Maud Rise; metals; nannofossils; Ocean Drilling Program; ODP Site 690; paleo-oceanography; Paleocene; paleoecology; Paleogene; Plantae; preservation; productivity; Southern Ocean; Sr/Ca; strontium; Tertiary; Weddell Sea;

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