Rapid shifts in South American montane climates driven by pCO<sub>2</sub> and ice volume changes over the last two glacial cycles

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Rapid shifts in South American montane climates driven by pCO₂ and ice volume changes over the last two glacial cycles

机译：在过去两个冰川周期中，pCO _{2 和冰量的变化驱动了南美山地气候的快速变化}

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《Climate of the Past Discussions》 |2010年第2期|共2页
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1. Rapid shifts in South American montane climates driven by pCO₂ and ice volume changes over the last two glacial cycles [J] . Climate of the Past Discussions . 2010,第4期

机译：在过去两个冰川周期中，pCO _{2 和冰量的变化驱动了南美山地气候的快速变化}
2. Rapid shifts in South American montane climates driven by pCO₂ and ice volume changes over the last two glacial cycles [J] . M. H. M. Groot, R. G. Bogotá, L. J. Lourens, Climate of the Past Discussions . 2010,第6期

机译：在过去两个冰川周期中，pCO _{2 驱动的南美山地气候快速变化和冰量变化}
3. Rapid shifts in South American montane climates driven by pCO₂ and ice volume changes over the last two glacial cycles [J] . Climate of the Past Discussions . 2010,第5期

机译：在过去两个冰川周期中，pCO _{2 和冰量的变化驱动了南美山地气候的快速变化}
4. Character of rapid vegetation and climate change during the late-giacial in southernmost South America [C] . Ray Kenny, Vera Markgraf NATO Advanced Research Workshop "Past and Future Rapid Environmental Changes: The Spatial and Evolutionary Responses of Terrestrial Biota" . 1997

机译：南美南美南美洲晚吉龙期间快速植被和气候变化的性质
5. Rapid climate change in the tropical Americas during the late-glacial interval and the Holocene. [D] . Stansell, Nathan D. 2009

机译：晚冰川期和全新世期间热带美洲的快速气候变化。
6. Sea ice variability in the southern Norwegian Sea during glacial Dansgaard-Oeschger climate cycles [O] . Henrik Sadatzki, Trond M. Dokken, Sarah M. P. Berben, 2019

机译：冰川南丹斯加德-厄施格气候周期在挪威南部海冰的变化
7. Rapid shifts in South American montane climates driven by pCO2 and ice volume changes over the last two glacial cycles [O] . Groot, M. H. M., Bogotá, R. G., Lourens, L. J., 2010

机译：在过去两个冰川周期中，由pCO2和冰量变化驱动的南美山地气候快速变化

Rapid shifts in South American montane climates driven by pCO2 and ice volume changes over the last two glacial cycles

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Rapid shifts in South American montane climates driven by pCO₂ and ice volume changes over the last two glacial cycles