Hibbert F D, Williams F H, Fallon S J, Rohling E J
Research School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia.
Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton SO14 3ZH, UK.
Sci Data. 2018 May 29;5:180088. doi: 10.1038/sdata.2018.88.
The last deglacial was an interval of rapid climate and sea-level change, including the collapse of large continental ice sheets. This database collates carefully assessed sea-level data from peer-reviewed sources for the interval 0 to 25 thousand years ago (ka), from the Last Glacial Maximum to the present interglacial. In addition to facilitating site-specific reconstructions of past sea levels, the database provides a suite of data beyond the range of modern/instrumental variability that may help hone future sea-level projections. The database is global in scope, internally consistent, and contains U-series and radiocarbon dated indicators from both biological and geomorpohological archives. We focus on far-field data (i.e., away from the sites of the former continental ice sheets), but some key intermediate (i.e., from the Caribbean) data are also included. All primary fields (i.e., sample location, elevation, age and context) possess quantified uncertainties, which-in conjunction with available metadata-allows the reconstructed sea levels to be interpreted within both their uncertainties and geological context.
末次冰消期是气候和海平面快速变化的一个时期,包括大型大陆冰盖的崩塌。该数据库整理了来自同行评审资料的经过仔细评估的海平面数据,数据涵盖0至25千年前(ka)这一区间,即从末次盛冰期到当前的间冰期。除了便于针对特定地点重建过去的海平面外,该数据库还提供了一系列超出现代/仪器测量变化范围的数据,这可能有助于完善未来的海平面预测。该数据库范围覆盖全球,内部一致,包含来自生物和地貌档案的铀系和放射性碳测年指标。我们专注于远场数据(即远离 former continental ice sheets 的地点),但也纳入了一些关键的中间数据(即来自加勒比地区的数据)。所有主要字段(即样本位置、海拔、年龄和背景)都具有量化的不确定性,这些不确定性与可用的元数据一起,使得重建的海平面能够在其不确定性和地质背景中得到解释。 注:原文中“former continental ice sheets”表述似乎不太准确,可能影响对整体内容的精准理解。