基于比提尼亚运算的英国四年制的时间框架
Kirsty E H Penkman1, Richard C Preece, David R Bridgland
1BioArCh, Department of Archaeology, University of York, York YO10 5DD, UK. kirsty.penkman@york.ac.uk
Nature
|August 2, 2011
概括
使用胃类动物操作体的氨基基层图谱为英国四季纪的序列提供了强大的时间线. 这种方法将陆地记录与海洋同位素阶段联系起来,揭示了人类在整个冰川和冰川间周期的占用模式.
科学领域:
- 古气候学 古气候学
- 四季地质地质学四季地质地质学
- 生物分层学是生物分层学.
背景情况:
- 地球的四季期具有循环的冰川和间冰川,挑战了陆地记录的相关性.
- 氨基层谱学提供了一种潜在的方法,可以使陆地序列与海洋同位素阶段 (MIS) 保持一致.
研究的目的:
- 开发一个综合的aminostratigraphy为英国的普世使用淡水类操作器.
- 建立一个强大的约会框架,为四次地球序列.
主要方法:
- 在74个英国地点的470个操作体中分析了氨基酸降解 (Asx,Glx,Ser,Ala,Val).
- 基于蛋白质降解程度的相对年龄排名.
主要成果:
- 建立了一种新的氨基层学法,与现有的层学数据相一致.
- 在英格兰 (MIS 12) 和全新纪之间的四个冰河间阶段得到证实.
- 在MIS 15后的冰河间阶段发现了英国的人类居住,在MIS 5e期间没有人居住.
- 证实Upton Warren间阶段最佳值是MIS 3之前的.
结论:
- 新的氨基层学为四年制研究提供了可靠的框架.
- 支持详细重建过去的气候,生物层级学和考古事件.
- 改进了对四年纪关键时期人类存在和缺席的理解.
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