Department of Geosciences, Princeton University, Princeton, NJ 08544.
Max Planck Institute for Chemistry, Mainz 55128, Germany.
Proc Natl Acad Sci U S A. 2023 Jan 3;120(1):e2206742119. doi: 10.1073/pnas.2206742119. Epub 2022 Dec 27.
The cyclic growth and decay of continental ice sheets can be reconstructed from the history of global sea level. Sea level is relatively well constrained for the Last Glacial Maximum (LGM, 26,500 to 19,000 y ago, 26.5 to 19 ka) and the ensuing deglaciation. However, sea-level estimates for the period of ice-sheet growth before the LGM vary by > 60 m, an uncertainty comparable to the sea-level equivalent of the contemporary Antarctic Ice Sheet. Here, we constrain sea level prior to the LGM by reconstructing the flooding history of the shallow Bering Strait since 46 ka. Using a geochemical proxy of Pacific nutrient input to the Arctic Ocean, we find that the Bering Strait was flooded from the beginning of our records at 46 ka until [Formula: see text] ka. To match this flooding history, our sea-level model requires an ice history in which over 50% of the LGM's global peak ice volume grew after 46 ka. This finding implies that global ice volume and climate were not linearly coupled during the last ice age, with implications for the controls on each. Moreover, our results shorten the time window between the opening of the Bering Land Bridge and the arrival of humans in the Americas.
大陆冰盖的周期性生长和衰减可以从全球海平面的历史中重建。对于末次冰盛期(LGM,距今 26500 至 19000 年前,26.5 至 19 千年前)及其随后的冰消期,海平面的估计相对较好。然而,LGM 之前冰盖生长期间的海平面估计值差异超过 60 米,这一不确定性与当代南极冰盖的海平面当量相当。在这里,我们通过重建 46 千年前以来浅贝加尔海峡的洪水历史来限制 LGM 之前的海平面。利用太平洋营养物质输入北冰洋的地球化学示踪剂,我们发现从我们的记录开始于 46 千年前,直到[公式:见正文]千年前,白令海峡一直被淹没。为了匹配这一洪水历史,我们的海平面模型要求冰期历史中,超过 50%的 LGM 全球峰值冰量是在 46 千年前之后增长的。这一发现意味着在上一个冰河时代,全球冰量和气候之间没有线性耦合,这对它们各自的控制因素都有影响。此外,我们的结果缩短了白令陆桥开放和人类到达美洲之间的时间窗口。