Arid
DOI10.1073/pnas.1909165116
Subglacial meltwater supported aerobic marine habitats during Snowball Earth
Lechte, Maxwell A.1,2; Wallace, Malcolm W.1; Hood, Ashleigh van Smeerdijk1; Li, Weiqiang3; Jiang, Ganqing4; Halverson, Galen P.2; Asael, Dan5; McColl, Stephanie L.1; Planavsky, Noah J.5
通讯作者Lechte, Maxwell A.
来源期刊PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
ISSN0027-8424
出版年2019
卷号116期号:51页码:25478-25483
英文摘要The Earth's most severe ice ages interrupted a crucial interval in eukaryotic evolution with widespread ice coverage during the Cryogenian Period (720 to 635 Ma). Aerobic eukaryotes must have survived the Snowball Earth glaciations, requiring the persistence of oxygenated marine habitats, yet evidence for these environments is lacking. We examine iron formations within globally distributed Cryogenian glacial successions to reconstruct the redox state of the synglacial oceans. Iron isotope ratios and cerium anomalies from a range of glaciomarine environments reveal pervasive anoxia in the ice-covered oceans but increasing oxidation with proximity to the ice shelf grounding line. We propose that the outwash of subglacial meltwater supplied oxygen to the synglacial oceans, creating glaciomarine oxygen oases. The confluence of oxygen-rich meltwater and iron-rich seawater may have provided sufficient energy to sustain chemosynthetic communities. These processes could have supplied the requisite oxygen and organic carbon source for the survival of early animals and other eukaryotic heterotrophs through these extreme glaciations.
英文关键词oxygenation glaciation Snowball Earth iron formation Fe isotopes
类型Article
语种英语
国家Australia ; Canada ; Peoples R China ; USA
开放获取类型Green Published, Bronze
收录类别SCI-E
WOS记录号WOS:000503281500025
WOS关键词KINGSTON PEAK FORMATION ; IRON-FORMATION ; ICE SHELF ; FE ISOTOPE ; DYNAMICS ; CONSTRAINTS ; SPONGES ; ORIGIN ; RECORD ; SHEET
WOS类目Multidisciplinary Sciences
WOS研究方向Science & Technology - Other Topics
EI主题词2019-12-17
来源机构南京大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/311820
作者单位1.Univ Melbourne, Sch Earth Sci, Parkville, Vic 3010, Australia;
2.McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 0E8, Canada;
3.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210093, Jiangsu, Peoples R China;
4.Univ Nevada, Dept Geosci, Las Vegas, NV 89154 USA;
5.Yale Univ, Dept Geol & Geophys, New Haven, CT 06511 USA
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GB/T 7714
Lechte, Maxwell A.,Wallace, Malcolm W.,Hood, Ashleigh van Smeerdijk,et al. Subglacial meltwater supported aerobic marine habitats during Snowball Earth[J]. 南京大学,2019,116(51):25478-25483.
APA Lechte, Maxwell A..,Wallace, Malcolm W..,Hood, Ashleigh van Smeerdijk.,Li, Weiqiang.,Jiang, Ganqing.,...&Planavsky, Noah J..(2019).Subglacial meltwater supported aerobic marine habitats during Snowball Earth.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,116(51),25478-25483.
MLA Lechte, Maxwell A.,et al."Subglacial meltwater supported aerobic marine habitats during Snowball Earth".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 116.51(2019):25478-25483.
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