整个冰期斯图尔特雪球冰川的粘土矿物地球化学和古环境重建

IF 3.2 2区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Jalila Al Bahri , Olabode Bankole , Duncan Muir , Abderrazzak El Albani , Anthony Oldroyd , Diana Contreras , Morten Andersen , Ernest Chi Fru
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引用次数: 0

摘要

最近从海洋沉积岩中获得的证据表明,在距今 7.17-6.6 亿年前的斯图尔特雪球地球冰川末期,粘土矿物对海水中生物必需营养物质的供应非常重要。然而,人们对这些粘土矿物的特征、它们在冰川前、冰川期和冰川后沉积物中的丰度和分布知之甚少。在这里,高分辨率岩相扫描电子显微镜-能量色散 X 射线光谱分析,结合大块和 2µ 粘土尺寸分数 X 射线衍射矿物学分析以及痕量和主要元素地球化学分析,表明在苏格兰艾莱岛和加维尔拉克斯岛保存的整个斯特尔蒂雪球地层的浅海平台沉积物中主要富含伊利石。冰川沉积物中富含绿泥石,而在冰川前和冰川后温室面层中观察到孔隙填充自生高岭石,但在冰川成因沉积物中却很少见。Th/Sc与Zr/Sc比率的二元判别图表明,水力分选和循环过程对原始沉积物成分的改变不大,再加上化学风化指数,表明前冰期和后冰期源岩的化学风化程度为中等至强烈。较低的化学交替指数(CIA)值,加上冰川淤积物中明显的绿泥石成分,与雪球末期融化冰原对大陆地块的机械耕作是一致的。冰川前和冰川后沉积物的中等至强烈化学风化指数与大气中二氧化碳含量和温度升高的温室条件相吻合。总体而言,粘土矿物主要来源于碎屑岩,这意味着冰川期后的营养物质供应增强,在运输过程中与 pH 值较低的河水中的粘土矿物结合,然后在 pH 值较高的盐海水中释放出来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Clay mineral geochemistry and paleoenvironmental reconstruction across the Cryogenian Sturtian Snowball glaciation

Clay mineral geochemistry and paleoenvironmental reconstruction across the Cryogenian Sturtian Snowball glaciation

Recent evidence from marine sedimentary rocks suggests that clay minerals were important in the supply of bioessential nutrients to seawater at the end of the Sturtian Snowball Earth glaciation that occurred ∼ 717–660 million years ago. However, little is known about the identity of these clay minerals, their abundance and distribution in the pre-glacial, glacial and post-glacial deposits. Here, high resolution petrographic scanning electron microscopy-energy dispersive x-ray spectroscopy, combined with bulk and < 2µ clay-size fraction X-ray diffraction mineralogical analysis and trace and major element geochemistry, point to dominant enrichment of illite in shallow marine platform sediments preserved across Sturtian Snowball Earth facies on Islay and the Garvellachs Island, Scotland. The glacial till is enriched with detrital chlorite, while pore-filling authigenic kaolinite is observed in the pre-glacial and post-glacial greenhouse facies, but scarce in the glaciogenic tillites. Discriminant binary plots of Th/Sc vs Zr/Sc ratios, indicative of insignificant modification of primary sediment composition by hydraulic sorting and recycling processes, together with chemical weathering indices, point to moderate to intense chemical weathering of the pre-glacial and post-glacial source rocks. Low Chemical Index of Alternation (CIA) values, coupled to the distinct chlorite composition of the glacial till, is consistent with mechanical tillage of continental landmass by the terminal Snowball melting ice sheets. The moderate to intense chemical weathering indices in the pre- and post-glacial deposits correspond with greenhouse conditions of elevated atmospheric CO2 content and temperature. Overall, the predominantly detrital origin of the clay minerals implies enhanced post-glacial nutrient supply bound to clay minerals in lower pH river water during transportation, followed by release in higher pH saline seawater.

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来源期刊
Precambrian Research
Precambrian Research 地学-地球科学综合
CiteScore
7.20
自引率
28.90%
发文量
325
审稿时长
12 months
期刊介绍: Precambrian Research publishes studies on all aspects of the early stages of the composition, structure and evolution of the Earth and its planetary neighbours. With a focus on process-oriented and comparative studies, it covers, but is not restricted to, subjects such as: (1) Chemical, biological, biochemical and cosmochemical evolution; the origin of life; the evolution of the oceans and atmosphere; the early fossil record; palaeobiology; (2) Geochronology and isotope and elemental geochemistry; (3) Precambrian mineral deposits; (4) Geophysical aspects of the early Earth and Precambrian terrains; (5) Nature, formation and evolution of the Precambrian lithosphere and mantle including magmatic, depositional, metamorphic and tectonic processes. In addition, the editors particularly welcome integrated process-oriented studies that involve a combination of the above fields and comparative studies that demonstrate the effect of Precambrian evolution on Phanerozoic earth system processes. Regional and localised studies of Precambrian phenomena are considered appropriate only when the detail and quality allow illustration of a wider process, or when significant gaps in basic knowledge of a particular area can be filled.
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