globalchange  > 气候变化与战略
DOI: 10.5194/cp-11-1009-2015
Scopus记录号: 2-s2.0-84938504291
论文题名:
The Paleocene-Eocene Thermal Maximum at DSDP Site 277, Campbell Plateau, southern Pacific Ocean
作者: Hollis C.J.; Hines B.R.; Littler K.; Villasante-Marcos V.; Kulhanek D.K.; Strong C.P.; Zachos J.C.; Eggins S.M.; Northcote L.; Phillips A.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2015
卷: 11, 期:7
起始页码: 1009
结束页码: 1025
语种: 英语
Scopus关键词: alkaline earth metal ; carbon isotope ; Eocene ; foraminifera ; hiatus ; nanofossil ; oceanic circulation ; Paleocene ; Paleocene-Eocene boundary ; paleolatitude ; sediment core ; temperature effect ; water temperature ; Campbell Plateau ; Pacific Ocean ; Pacific Ocean (South)
英文摘要: Re-examination of sediment cores from Deep Sea Drilling Project (DSDP) Site 277 on the western margin of the Campbell Plateau (paleolatitude of ∼65°S) has identified an intact Paleocene-Eocene (P-E) boundary overlain by a 34 cm thick record of the Paleocene-Eocene Thermal Maximum (PETM) within nannofossil chalk. The upper part of the PETM is truncated, either due to drilling disturbance or a sedimentary hiatus. An intact record of the onset of the PETM is indicated by a gradual decrease in δ13C values over 20 cm, followed by a 14 cm interval in which δ13C is 2‰ lighter than uppermost Paleocene values. After accounting for effects of diagenetic alteration, we use δ18O and Mg/Ca values from foraminiferal tests to determine that intermediate and surface waters warmed by ∼5-6° at the onset of the PETM prior to the full development of the negative δ13C excursion. After this initial warming, sea temperatures were relatively stable through the PETM but declined abruptly across the horizon that truncates the event at this site. Mg/Ca analysis of foraminiferal tests indicates peak intermediate and surface water temperatures of ∼19 and ∼32°C, respectively. These temperatures may be influenced by residual diagenetic factors and changes in ocean circulation, and surface water values may also be biased towards warm-season temperatures. © Author(s) 2015.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49128
Appears in Collections:气候变化与战略

Files in This Item:

There are no files associated with this item.


Recommended Citation:
Hollis C.J.,Hines B.R.,Littler K.,et al. The Paleocene-Eocene Thermal Maximum at DSDP Site 277, Campbell Plateau, southern Pacific Ocean[J]. Climate of the Past,2015-01-01,11(7)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Hollis C.J.]'s Articles
[Hines B.R.]'s Articles
[Littler K.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Hollis C.J.]'s Articles
[Hines B.R.]'s Articles
[Littler K.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Hollis C.J.]‘s Articles
[Hines B.R.]‘s Articles
[Littler K.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.