The last deglacial sea-level and climatic changes. Coral Reef records in the south Pacific : Tahiti (French Polynesia) - IODP Expedition #310 -, Australian Great Barrier Reef - IODP Proposal #519: Potential of diagenetically altered corals for sub-seasona

末次冰消期海平面与气候变化。

• 批准号: 35880301
• 负责人: Professor Dr. Wolf-Christian Dullo
• 金额: --
• 依托单位: GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
• 依托单位国家: 德国
• 项目类别: Research Grants
• 财政年份: 2007
• 资助国家: 德国
• 起止时间: 2006-12-31 至 2010-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/35880301?language=en
• 关键词: last; deglacial; sea; level; climatic

The timing and course of the last deglaclation (23.000-6,000 calendar years BP - cal. yr BP) are essential components for understanding the dynamics of large Ice sheets and their effects on Earth's isostasy as well as the complex relationship between freshwater fluxes to the ocean, thermohaline circulation and, hence, global climate during the Late Pleistocene and the Holocene. This proposal Is related to the IODP proposal #519 concerning the coral reef records of Tahiti and the Australian Great Barrier Reef to establish the course of sea-level rise, climate variability and reef response during the last deglaciatton. It includes : 1) the study of more than 600 m of reef cores with an exceptional recovery that were retrieved from 37 holes ranging from 40 to 120 m water depth around Tahiti during the IODP Expedition 0310 « Tahiti Sea Level ». Distinctive levels of relict reefs covering most, if not all, the last deglaciation were drilled and therefore confirmed the significance of these features as unique archives of abrupt global sea-level rise and climate change. 2) Complimentary investigations of the Tahiti reef slopes, and 3) a site survey cruise on the Great Barrier Reef to generate high resolution bathymetric and seismic data that will be used to select suitable targets for an IODP drilling expedition corresponding to the part 2 of the IODP drilling proposal #519. The general scientific objectives of this proposal are threefold :a. To establish the course of post-glacial sea-level rise during the Last Deglaclation .b. To define SSTs and SSSs variations during the Last Deglaciation when solar insolation, sea level, and atmospheric CO2 levels were different from today. c. To analyze the impact of sea-level and environmental changes on reef development during the Last Deglaciation, with a special emphasis on the comprehensive reconstruction of environmental changes.

最后一次冰川消融的时间和过程（23.000- 6，000日历年BP - cal. yr BP）是了解大冰盖动态及其对地球等渗线的影响以及晚更新世和全新世期间淡水流入海洋、温盐环流和全球气候之间复杂关系的重要组成部分。该提案与IODP关于塔希提岛和澳大利亚大堡礁珊瑚礁记录的第519号提案有关，以确定最后一次冰消期间海平面上升、气候变化和珊瑚礁反应的过程。它包括：1） 在IODP Expedition 0310 « Tahiti Sea Level »期间，从大溪地周围水深40至120米的37个钻孔中回收了600多米的珊瑚礁岩心，并对其进行了研究。对覆盖最后一次冰消期的大部分（如果不是全部的话）残礁的独特水平进行了钻探，因此证实了这些特征作为全球海平面突然上升和气候变化的独特档案的重要性。（二） 大溪地礁坡的免费调查，以及3） 对大堡礁进行现场勘测巡航，以生成高分辨率测深和地震数据，这些数据将用于为IODP钻探勘探选择合适的目标，该钻探勘探与IODP钻探建议书#519第2部分相对应。该提案的总体科学目标有三个方面：a.确定末次冰川消融期间冰后期海平面上升的过程。在末次冰消期，当太阳辐射、海平面和大气CO2水平与今天不同时，确定SST和SSSS的变化。C.分析末次冰消期海平面和环境变化对生物礁发育的影响，特别强调环境变化的综合重建。