Recognition of alkenones in a lower Aptian porcellanite from the west-central Pacific

被引:49
作者
Brassell, SC [1 ]
Dumitrescu, M [1 ]
机构
[1] Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
基金
美国国家科学基金会;
关键词
D O I
10.1016/j.orggeochem.2003.09.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 [地球物理学]; 070902 [地球化学];
摘要
ODP Leg 198 drilling on Shatsky Rise recovered a lower Aptian porcellanite (similar to 120.5 Ma) deposited during oceanic anoxic event (OAE) la that contains C-36-C-39 alkadienones: C-37:2 and C-39:2 alkadien-2-ones and C-36:2 and C-38:2 alkadien-3-ones. This alkenone distribution differs from that typical of contemporary sediments and haptophyte algae, but resembles that of Cretaceous sediments from the Blake-Bahama basin. The discovery of alkenones in the early Aptian extends their sedimentary record by 15 M.y. to 120.5 M.y. and demonstrates the potential for long-term survival of these diagnostic functional lipids under favorable depositional conditions and subsequent shallow burial. It also contributes to the understanding and reconstruction of evolutionary developments in alkenone distributions and biosynthesis over geologic time. (C) 2003 Elsevier Ltd. All rights reserved.
引用
收藏
页码:181 / 188
页数:8
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