The Quaternary is here to stay

被引:19
|
作者
Bowen, D. Q. [1 ]
Gibbard, Philip L.
机构
[1] Cardiff Univ, Sch Earth Ocean & Planetary Sci, Cardiff CF10 3YE, Wales
[2] Univ Cambridge, Dept Geog, Cambridge Quaternary, Cambridge, England
关键词
Quaternary; Pleistocene; classification; global stratigraphic timescale;
D O I
10.1002/jqs.1082
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The proposals to drop the name Quaternary, to extend the Neogene Period to the present day, and to confirm the base of the Pleistocene at 1.8 Ma are reviewed. it is concluded that there is no scientific case for dropping the name Quaternary and that an overwhelming volume of evidence points to 2.6Ma as the most appropriate base for the Quaternary/Pleistocene, when extensive Northern Hemisphere mid-latitude glaciation occurred under what were essentially similar physical boundary conditions of continents, oceans, seaways and mountain ranges that characterise, and are unique to, the Quaternary. It is desirable that all stratigraphical and geochronological evidence is tied rigorously into the Global Stratigraphic Timescale. Copyright (c) 2007 John Wiley & Sons, Ltd.
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页码:3 / 8
页数:6
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