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Northeast Greenland Speleothems Trap Forest Pollen During MIS

crossref(2024)

Cited 0|Views19
Abstract
Diminishing ice sheets, an intensification of the hydrological cycle, and shifts in vegetation composition and abundance, are some of the results of the Arctic’s amplified response to climate warming. Improved understanding of Arctic amplification can be achieved through investigation of past interglacial periods. Although an increasing number of studies exploring past interglacials in Greenland exist, northeastern Greenland remains under-investigated, despite being highly sensitive to the effects of Arctic amplification. Here, we investigate the palaeoenvironment under warmer and wetter climate conditions by using pollen trapped in speleothems that were deposited in northeastern Greenland (80°N, 22°W) during late Marine Isotope Stage (MIS) 11. The results are placed in the context of a sensitivity study into modern pollen compositions recorded in surface samples as well as published Holocene records from eastern and northern Greenland. The deposition of speleothems in northeastern Greenland during MIS 11 and the composition of the trapped pollen assemblages provide a first-order proxy for drastically different atmospheric and oceanic boundary conditions compared to today. Modern and Holocene pollen samples are dominated by open land vegetation (shrubs and herbs), whereas the MIS 11 speleothem-trapped pollen show an abundance of conifer trees, primarily fir and pine, as well as an array of deciduous trees, shrubs, and open land vegetation. These results are in agreement with findings from other studies investigating southern Greenland during MIS 11. The speleothems and trapped pollen used in this study thus provide direct terrestrial evidence for the presence of higher vegetation in northeastern Greenland during MIS 11 and indirectly help to constrain the extent of the ice sheet at that time.
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要点】:研究利用东北格陵兰岛 MIS 11 时期的洞穴沉积物中的花粉记录,揭示了当时气候变暖和植被变化的状况,为理解北极放大效应提供了新的证据。

方法】:通过分析东北格陵兰岛 MIS 11 时期洞穴中捕获的花粉组合,结合现代花粉组成和全新世记录,对比研究了过去气候和植被变化。

实验】:在东北格陵兰岛(80°N, 22°W)的洞穴中收集了 MIS 11 时期的洞穴沉积物,并对其中的花粉组成进行了分析,发现 MIS 11 时期的花粉组合与现代和全新世花粉组合存在显著差异,表明当时该地区植被更为丰富,包括大量针叶树和阔叶树。