Schreiber Lennart, Ribeiro Sofia, Jackson Rebecca, Kvorning Anna Bang, Nota Kevin, O'Regan Matt, Pearce Christof, Seersholm Frederik, Seidenkrantz Marit-Solveig, Zimmermann Heike H, Lorenzen Eline D
Globe Institute, University of Copenhagen, Copenhagen, Denmark.
Department of Glaciology and Climate, Geological Survey of Denmark and Greenland, Copenhagen, Denmark.
Nat Commun. 2025 May 15;16(1):4543. doi: 10.1038/s41467-025-59731-0.
Arctic marine ecosystems have undergone notable reconfigurations in response to Holocene climate and environmental changes. Yet our understanding of how marine mammal occurrence was impacted remains limited, due to their relative scarcity in the fossil record. We reconstruct the occurrence of marine mammals across the past 12,000 years through detections based on sedimentary ancient DNA from four marine sediment cores collected around Northern Greenland, and integrate the findings with local and regional environmental proxy records. Our findings indicate a close association between marine mammals at densities detectable in marine sediments and the deglaciation of high Arctic marine environments at the onset of the Holocene. Further, we identify air temperature and changes in sea ice cover as significant drivers of community change across time. Several marine mammals are detected in the sediments earlier than in the fossil record, for some species by several thousand years. During the Early-to-Mid Holocene, a period of warmer climate, we record northward distribution shifts of temperate and low-arctic marine mammal species. Our findings provide unique, long-term baseline data on the occurrence of marine mammals around Northern Greenland, enabling insights into past community dynamics and the effects of Holocene climatic shifts on the region's marine ecosystems.
北极海洋生态系统因全新世气候和环境变化而经历了显著的重新配置。然而,由于它们在化石记录中相对稀少,我们对海洋哺乳动物出现情况受何影响的了解仍然有限。我们通过对从格陵兰岛北部周围采集的四个海洋沉积岩芯中的沉积古代DNA进行检测,重建了过去12000年里海洋哺乳动物的出现情况,并将这些发现与当地和区域环境代理记录相结合。我们的研究结果表明,在海洋沉积物中可检测到的密度下的海洋哺乳动物与全新世开始时高北极海洋环境的冰消作用之间存在密切关联。此外,我们确定气温和海冰覆盖变化是不同时期群落变化的重要驱动因素。在沉积物中检测到的几种海洋哺乳动物比在化石记录中出现的时间更早,有些物种早了几千年。在全新世早期至中期,气候较为温暖的时期,我们记录到温带和低北极海洋哺乳动物物种向北分布的转移。我们的研究结果提供了关于格陵兰岛北部周围海洋哺乳动物出现情况的独特长期基线数据,有助于深入了解过去的群落动态以及全新世气候变化对该地区海洋生态系统的影响。