气候变化领域集成服务门户(CCPortal): Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene-Eocene Thermal Maximum

CCPortal

DOI	10.1029/2018GL080761
	Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene-Eocene Thermal Maximum
	Ilyina, Tatiana; Heinze, Mathias
发表日期	2019-01-28
ISSN	0094-8276
EISSN	1944-8007
卷号	46 期号:2 页码:842-852
英文摘要	The Paleocene-Eocene Thermal Maximum was a transient, carbon-induced global warming event, considered the closest analog to ongoing climate change. Impacts of a decrease in deepwater formation during the onset of the Paleocene-Eocene Thermal Maximum sugge
学科领域	Geosciences, Multidisciplinary
语种	英语
WOS记录号	WOS:000458607400035
来源期刊	GEOPHYSICAL RESEARCH LETTERS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/79787
作者单位	Max Planck Inst Meteorol, Hamburg, Germany
推荐引用方式 GB/T 7714	Ilyina, Tatiana,Heinze, Mathias. Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene-Eocene Thermal Maximum[J],2019,46(2):842-852.
APA	Ilyina, Tatiana,&Heinze, Mathias.(2019).Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene-Eocene Thermal Maximum.GEOPHYSICAL RESEARCH LETTERS,46(2),842-852.
MLA	Ilyina, Tatiana,et al."Carbonate Dissolution Enhanced by Ocean Stagnation and Respiration at the Onset of the Paleocene-Eocene Thermal Maximum".GEOPHYSICAL RESEARCH LETTERS 46.2(2019):842-852.