The Pleistocene footprints are younger than we thought: correcting the radiocarbon dates of Ruppia seeds, Tularosa Basin, New Mexico

IF 1.7 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
David M. Rachal, Robert Dello-Russo, Matthew Cuba
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引用次数: 0

Abstract

Past studies have demonstrated that Ruppia cirrhosa (Ruppia), which typically grows in brackish water, is far too unreliable to serve as the chronological basis for radiocarbon dating because of the hard water effect (HWE). Despite this unreliability, Ruppia seeds have been used to date footprints along the margins of paleo-Lake Otero in southern New Mexico to around 23,000–21,000 cal yr BP. In this study, we employ a modern analog approach using δ13C values and radiocarbon dates from modern Ruppia plants growing in Salt Creek to calculate a maximum limiting age range for the footprints. Those plant samples with higher δ13C values produced greater age discrepancies. This simple relationship can be used to correct for the HWE and demonstrates that the human footprints purported to have been made during the local last glacial maximum could be at least ~7500 yr younger.

更新世的脚印比我们想象的要年轻:校正新墨西哥州图拉罗萨盆地 Ruppia 种子的放射性碳年代
过去的研究表明,由于硬水效应(HWE),通常生长在咸水中的 Ruppia cirrhosa(Ruppia)作为放射性碳年代测定的年代学基础非常不可靠。尽管这种方法不可靠,但 Ruppia 种子还是被用来测定新墨西哥州南部古奥特罗湖边缘脚印的年代,大约为公元前 23,000-21,000 卡年。在这项研究中,我们采用了一种现代类比方法,利用生长在盐溪的现代茹贝藻植物的 δ13C 值和放射性碳年代来计算足迹的最大极限年龄范围。δ13C值较高的植物样本产生的年龄差异较大。这种简单的关系可用来校正 HWE,并证明据称是在当地末次冰川最盛时期留下的人类脚印至少比现在年轻约 7500 年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Quaternary Research
Quaternary Research 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
57
审稿时长
3 months
期刊介绍: Quaternary Research is an international journal devoted to the advancement of the interdisciplinary understanding of the Quaternary Period. We aim to publish articles of broad interest with relevance to more than one discipline, and that constitute a significant new contribution to Quaternary science. The journal’s scope is global, building on its nearly 50-year history in advancing the understanding of earth and human history through interdisciplinary study of the last 2.6 million years.
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