Mercia Mudstone群(英国德文郡)的磁地层学:对西欧中晚三叠世区域关系和时间地层学的影响

IF 2.6 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of the Geological Society Pub Date : 2023-04-28 DOI:10.1144/jgs2022-173
M. Hounslow, R. Gallois
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引用次数: 1

摘要

由于缺乏年代测定方法,在深部时间内全球同步陆地序列的环境变化具有挑战性,英国中上三叠世麦西亚泥岩群也适用这种情况。利用海岸悬崖剖面,对263个层位的磁地层学进行了评估,确定了53个磁带。该群下部140m的磁带显示出与Ladinian中期至Carnian早期极性时间尺度的磁带一致,测年与下伏Sherwood砂岩群的磁地层学一致。Dunscombe泥岩组的磁地层学和相关的孢粉学数据表明,卡尼阶晚期至诺里阶早期,其堆积速率明显低于相邻地层。极性记录显示了卡尼阶威塞克斯盆地和中欧盆地之间的同时代洪水事件、蒸发岩沉积和供沙间隔。这是这些独立盆地之间气候和海平面变化的结果,与风尘供应和超干旱细粒源区的缩小有关。Branscombe泥岩和Blue Anchor地层的磁地层学显示了它们的诺里阶和早期雷蒂阶。这些和其他数据表明,在北欧极性时间尺度上,海洋和非海洋极性记录可以进行替代同步。198字补充材料:采样剖面和推断序列边界的剖面细节和详细日志、磁性矿物学数据、退磁行为和平均方向、虚拟地磁极数据汇总和与其他欧洲磁极的比较、其他复合参考剖面的构建和修订的极性标度。Excel磁数据表对相关模型和年龄模型进行了统计评估。https://doi.org/10.6084/m9.figshare.c.6613788
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Magnetostratigraphy of the Mercia Mudstone Group (Devon, UK): implications for regional relationships and chronostratigraphy in the Middle to Late Triassic of western Europe
Global synchronisation of environmental change in terrestrial successions in deep-time is challenging due to the paucity of dating methods, a case also applicable to the Middle to Upper Triassic Mercia Mudstone Group in Britain. Using coastal cliff sections, magnetostratigraphy was evaluated at 263 horizons, defining 53 magnetozones. Magnetozones from the lower 140 m of the group demonstrate correspondence to those from the mid Ladinian to early Carnian polarity timescale, dating which is compatible with magnetostratigraphy from the underlying Sherwood Sandstone Group. Magnetostratigraphy of the Dunscombe Mudstone Formation, and associated palynological data, suggest a late Carnian to earliest Norian age, and a dramatically lower accumulation rate than adjacent formations. The polarity record demonstrates coeval flooding events, evaporite deposits and intervals of sand supply between the Wessex Basin and the Central European Basin in the Carnian. This is the result of linked climatic and eustatic changes between these separate basins, related to aeolian dust supply and the shrinkage of hyper-arid source regions for the fines. Magnetostratigraphy from the Branscombe Mudstone and Blue Anchor formations demonstrates their Norian and early Rhaetian age. These and other data suggest an alternative synchronization of marine and non-marine polarity records for the Norian polarity timescale. 198 words Supplementary material: Section details and detailed logs of the sampled sections and inferred sequence boundaries, magnetic mineralogy data, demagnetisation behaviour and mean directions, summary of virtual geomagnetic pole data and a comparison to other European poles, construction of other composite reference sections and revised polarity scales. Excel sheet of magnetic data statistically evaluated correlation models, and age models. https://doi.org/10.6084/m9.figshare.c.6613788
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来源期刊
Journal of the Geological Society
Journal of the Geological Society 地学-地球科学综合
CiteScore
6.00
自引率
3.70%
发文量
68
审稿时长
6-12 weeks
期刊介绍: Journal of the Geological Society (JGS) is owned and published by the Geological Society of London. JGS publishes topical, high-quality recent research across the full range of Earth Sciences. Papers are interdisciplinary in nature and emphasize the development of an understanding of fundamental geological processes. Broad interest articles that refer to regional studies, but which extend beyond their geographical context are also welcomed. Each year JGS presents the ‘JGS Early Career Award'' for papers published in the journal, which rewards the writing of well-written, exciting papers from early career geologists. The journal publishes research and invited review articles, discussion papers and thematic sets.
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