Oceanographic mechanisms and penguin population increases during the Little Ice Age in the southern Ross Sea, Antarctica
Oceanographic mechanisms and penguin population increases during the Little Ice Age in the southern Ross Sea, Antarctica
复制标题
南极洲罗斯海南部小冰河时期的海洋学机制和企鹅数量增加
DOI:
10.1016/j.epsl.2017.10.027
复制
发表时间:
2018-01-01
影响因子:
5.3
通讯作者:
Wang, Yuhong
中科院分区:
文献类型:
--
作者:
Yang, Lianjiao;Sun, Liguang;Wang, Yuhong
The Adelie penguin is a well-known indicator for climate and environmental changes. Exploring how large-scale climate variability affects penguin ecology in the past is essential for understanding the responses of Southern Ocean ecosystems to future global change. Using ornithogenic sediments at Cape Bird, Ross Island, Antarctica, we inferred relative population changes of Adelie penguins in the southern Ross Sea over the past 500 yr, and observed an increase in penguin populations during the Little Ice Age (LIA; 1500-1850 AD). We used cadmium content in ancient penguin guano as a proxy of ocean upwelling and identified a close linkage between penguin dynamics and atmospheric circulation and oceanic conditions. During the cold period of similar to 1600-1825 AD, a deepened Amundsen Sea Low (ASL) led to stronger winds, intensified ocean upwelling, enlarged Ross Sea and McMurdo Sound polynyas, and thus higher food abundance and penguin populations. We propose a mechanism linking Antarctic marine ecology and atmospheric/oceanic dynamics which can help explain and predict responses of Antarctic high latitudes ecosystems to climate change. (C) 2017 Elsevier B.V. All rights reserved.