Highly siderophile element and Re-Os isotope systematics of a Neoproterozoic Iron Formation and its temporal relation to glaciation events

IF 4.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Geochimica et Cosmochimica Acta Pub Date : 2024-09-18 DOI:10.1016/j.gca.2024.09.019
Tobias Prost , Toni Schulz , Sebastian Viehmann , Detlef H.G. Walde , Christian Koeberl
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Abstract

The Urucum iron- and manganese formation (IF-MnF) in the Santa Cruz Formation, Brazil, was deposited in a glacially influenced, late Neoproterozoic depositional environment. It has proven to be a reliable and robust archive for the late Neoproterozoic, allowing unique insights into the composition of seawater during an interval that is characterized by dramatic changes in the Earth’s litho-, hydros-, atmo-, and biosphere, including several episodes of low-latitude glaciations. Here we present highly siderophile element data of the Urucum IF-MnF to evaluate elemental sources that affected the Neoproterozoic seawater from which the Urucum IF-MnF precipitated. High uncertainties associated with current dating attempts of this formation overlapped with the Marinoan glaciation (∼650–635 Ma) as well as the Gaskiers glaciation event (∼580 Ma). A Re-Os regression line defined by iron-, manganese-, and chert-rich samples of the Urucum formation is interpreted as an isochron, yielding a refined age estimate of 577 ± 38 Ma and an initial 187Os/188Os ratio of 0.122 ± 0.003. The proposed depositional age overlaps with previous published age data of the Urucum IF-MnF, but relates the Urucum IF-MnF to the Ediacaran Gaskiers glaciation and overlaps with the age of the Shuram CIE (∼567 Ma). An initial 187Os/188Os ratio of 0.122 ± 0.003 is interpreted to represent pristine Neoproterozoic seawater and supports strong hydrothermal input, probably related to rifting, that promoted ferruginous conditions in the Urucum seawater.
In an alternative scenario, Re-Os isotope data for the Urucum IF-MnF could also be interpreted in a multi-component mixing scenario, defined by hydrothermally influenced water masses that sourced most metals within the Urucum basin and a crustal component that entered the Urucum seawater either as detrital admixture or via riverine loads. Although none of the scenarios can be ruled out, we consider the isochron scenario as more plausible.
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新近新生代铁地层的高亲铁元素和Re-Os同位素系统学及其与冰川事件的时间关系
巴西圣克鲁斯地层(Santa Cruz Formation)中的Urucum铁锰地层(IF-MnF)沉积于受冰川影响的新近纪晚期沉积环境中。事实证明,它是新近纪晚期可靠而稳健的档案,可以让人们对这一时期的海水成分有独特的了解,而这一时期的特点是地球的岩石圈、水圈、大气圈和生物圈都发生了巨大变化,包括几次低纬度冰川期。在这里,我们展示了乌鲁古姆 IF-MnF 的高嗜钠元素数据,以评估影响乌鲁古姆 IF-MnF 沉淀的新近纪海水的元素来源。目前对这一地层进行的测年尝试具有很高的不确定性,它与马里诺冰川(650-635 Ma)以及加斯基尔冰川(580 Ma)事件重叠。由Urucum地层中富含铁、锰和白垩系的样本定义的Re-Os回归线被解释为等时线,得出的细化年龄估计为577 ± 38 Ma,初始187Os/188Os比率为0.122 ± 0.003。所提出的沉积年龄与之前公布的Urucum IF-MnF年龄数据重叠,但将Urucum IF-MnF与埃迪卡拉纪的Gaskiers冰川作用联系起来,并与Shuram CIE的年龄(∼567 Ma)重叠。最初的 187Os/188Os 比率为 0.122 ± 0.003,被解释为代表原始的新新生代海水,并支持强烈的热液输入,可能与断裂有关,促进了乌鲁库姆海水的铁锈化条件。在另一种情况下,乌鲁库姆 IF-MnF 的 Re-Os 同位素数据也可以用多组分混合情况来解释,即受热液影响的水团,其大部分金属来源于乌鲁库姆海盆,而地壳组分则以碎屑混合物或通过河流负荷进入乌鲁库姆海水。虽然不能排除上述任何一种情况,但我们认为等时线情况更为可信。
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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