A millennium of climatic and floristic dynamics in the Eastern Cordillera of the Colombian Andes
A millennium of climatic and floristic dynamics in the Eastern Cordillera of the Colombian Andes
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DOI：
10.1111/jbi.14347
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发表时间：
2022-03
影响因子：
3.9
通讯作者：
A. Correa-Metrio;J. Escobar;B. Bird;Dayenari Caballero‐Rodriguez;B. Steinman;Paula A. Rodríguez-Zorro;J. Curtis
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作者：
A. Correa-Metrio;J. Escobar;B. Bird;Dayenari Caballero‐Rodriguez;B. Steinman;Paula A. Rodríguez-Zorro;J. Curtis
从中世纪气候异常（MCA，950-1250 CE）到小冰期（LIA，1350-1800 CE）的转变是过去两千年来最大的工业化前气候变化，为研究植被如何应对快速气候变化提供了机会。我们分析了沉积记录从哥伦比亚安第斯山脉重建区域植被动态在这段时间内，确定现代环境分布的化石记录中存在的类群和现代区域温度变化提供参考。
The transition from the Medieval Climate Anomaly (MCA, 950–1250 CE) to the Little Ice Age (LIA, 1350–1800 CE) is the largest pre‐industrial climate shift within the last two millennia, offering an opportunity to study how vegetation responds to rapid climate change. We analysed a sedimentary record from the Colombian Andes to reconstruct regional vegetation dynamics during this time interval, identify the modern environmental distribution of taxa present in the fossil record and provide a reference for modern regional temperature change.