Collaborative Research: Resolving Centennial-Scale Environmental Change and Geomagnetic Field Variability From Iberian Margin Sediment Drifts Cored on IODP Expedition 339

该提案旨在将连续 u 通道和离散古地磁数据与颜色分析和船载数据相结合，以开发 IODP 实验期间取芯的第四纪等高线剖面的年代和气候数据。 339. 磁数据将使第四纪地磁场变化的详细区域类型部分得以发展，这对地质年代学和有关磁场和地球发电机性质的更大问题都有影响。实验期间核心的五个站点。 339 将被检查，初步数据表明磁特性可以从孔到孔相关。第四纪记录的厚度和总体高沉积速率可能使这些岩心特别适合此类详细分析。这项研究与同位素、天文学和地层分析相结合，将能够构建极其详细的年代学，然后将其与气候模型，特别是与温盐环流相关的气候模型联系起来。这与exp的主要目标直接相关。 339 这是将地中海盐分流出与气候变化和事件相关的模型的开发和约束。在现代大西洋，这种流出对深海水循环具有重要影响。了解这些环流模式是预测全球气候变化的重要因素之一。

This proposal seeks to use continuous u-channel and discrete paleomagnetic data in combination with color analysis and shipboard data to develop chronological and climate data on the Quaternary contourite section cored during IODP exp. 339.The magnetic data will enable development of a detailed regional type section of Quaternary geomagnetic field variability with implications for both geochronology and larger questions concerning the nature of the magnetic field and geodynamo. Five sites cored during exp. 339 will be examined and preliminary data suggests that magnetic properties can be correlated from hole-to-hole. The thickness of the Quaternary record and overall high sedimentation rates could make these cores particularly amenable to this type of detailed analysis. This study, in combination with isotopic, astronomic, and stratigraphic analysis will enable construction of an exceptionally detailed chronology which can then be tied to climate models, especially those related to thermohaline circulation. This is directly related to the primary objective of exp. 339 which is the development and constraint of models relating saline Mediterranean outflow to climate variations and events. In the modern Atlantic, this outflow has important effects of the circulation of deep ocean water. The understanding of these circulation patterns is one important element of predicting global climate variations.