Earth's youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean

It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history. This view represents a major shift in our understanding of the evolution of marine chemistry. However, thus far, evidence for ferruginous conditions comes predominantly from Fe-s...

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Published inScientific reports Vol. 8; no. 1; pp. 9970 - 10
Main Authors Li, Zhi-Quan, Zhang, Lian-Chang, Xue, Chun-Ji, Zheng, Meng-Tian, Zhu, Ming-Tian, Robbins, Leslie J, Slack, John F, Planavsky, Noah J, Konhauser, Kurt O
Format Journal Article
LanguageEnglish
Published England Nature Publishing Group 02.07.2018
Nature Publishing Group UK
Subjects
Geological time
Iron
Marine environment
Sediments
Speciation
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Abstract It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history. This view represents a major shift in our understanding of the evolution of marine chemistry. However, thus far, evidence for ferruginous conditions comes predominantly from Fe-speciation data. Given debate over these records, new evidence for Fe-rich marine conditions is a requisite if we are to shift our view regarding evolution of the marine redox landscape. Here we present strong evidence for ferruginous conditions by describing a suite of Fe-rich chemical sedimentary rocks-banded iron formation (BIF)--deposited during the Early Cambrian in western China. Specifically, we provide new U-Pb geochronological data that confirm a depositional age of ca. 527 Ma for this unit, as well as rare earth element (REE) data are consistent with anoxic deposition. Similar to many Algoma-type Precambrian iron formations, these Early Cambrian sediments precipitated in a back-arc rift basin setting, where hydrothermally sourced iron drove the deposition of a BIF-like protolith, the youngest ever reported of regional extent without direct links to volcanogenic massive sulphide (VMS) deposits. Their presence indicates that marine environments were still characterized by chemical- and redox-stratification, thus supporting the view that-despite a dearth of modern marine analogues-ferruginous conditions continued to locally be a feature of early Phanerozoic seawater.
AbstractList It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history. This view represents a major shift in our understanding of the evolution of marine chemistry. However, thus far, evidence for ferruginous conditions comes predominantly from Fe-speciation data. Given debate over these records, new evidence for Fe-rich marine conditions is a requisite if we are to shift our view regarding evolution of the marine redox landscape. Here we present strong evidence for ferruginous conditions by describing a suite of Fe-rich chemical sedimentary rocks-banded iron formation (BIF)--deposited during the Early Cambrian in western China. Specifically, we provide new U-Pb geochronological data that confirm a depositional age of ca. 527 Ma for this unit, as well as rare earth element (REE) data are consistent with anoxic deposition. Similar to many Algoma-type Precambrian iron formations, these Early Cambrian sediments precipitated in a back-arc rift basin setting, where hydrothermally sourced iron drove the deposition of a BIF-like protolith, the youngest ever reported of regional extent without direct links to volcanogenic massive sulphide (VMS) deposits. Their presence indicates that marine environments were still characterized by chemical- and redox-stratification, thus supporting the view that-despite a dearth of modern marine analogues-ferruginous conditions continued to locally be a feature of early Phanerozoic seawater.
It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history . This view represents a major shift in our understanding of the evolution of marine chemistry . However , thus far , evidence for ferruginous conditions comes predominantly from Fe-speciation data . Given debate over these records , new evidence for Fe-rich marine conditions is a requisite if we are to shift our view regarding evolution of the marine redox landscape . Here we present strong evidence for ferruginous conditions by describing a suite of Fe-rich chemical sedimentary rocks—banded iron formation (BIF)—-deposited during the Early Cambrian in western China . Specifically , we provide new U-Pb geochronological data that confirm a depositional age of ca . 527 Ma for this unit , as well as rare earth element (REE) data are consistent with anoxic deposition . Similar to many Algoma-type Precambrian iron formations , these Early Cambrian sediments precipitated in a back-arc rift basin setting , where hydrothermally sourced iron drove the deposition of a BIF-like protolith , the youngest ever reported of regional extent without direct links to volcanogenic massive sulphide (VMS) deposits . Their presence indicates that marine environments were still characterized by chemical- and redox-stratification , thus supporting the view that—despite a dearth of modern marine analogues—ferruginous conditions continued to locally be a feature of early Phanerozoic seawater .
Abstract It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history . This view represents a major shift in our understanding of the evolution of marine chemistry . However , thus far , evidence for ferruginous conditions comes predominantly from Fe-speciation data . Given debate over these records , new evidence for Fe-rich marine conditions is a requisite if we are to shift our view regarding evolution of the marine redox landscape . Here we present strong evidence for ferruginous conditions by describing a suite of Fe-rich chemical sedimentary rocks—banded iron formation (BIF)—-deposited during the Early Cambrian in western China . Specifically , we provide new U-Pb geochronological data that confirm a depositional age of ca . 527 Ma for this unit , as well as rare earth element (REE) data are consistent with anoxic deposition . Similar to many Algoma-type Precambrian iron formations , these Early Cambrian sediments precipitated in a back-arc rift basin setting , where hydrothermally sourced iron drove the deposition of a BIF-like protolith , the youngest ever reported of regional extent without direct links to volcanogenic massive sulphide (VMS) deposits . Their presence indicates that marine environments were still characterized by chemical- and redox-stratification , thus supporting the view that—despite a dearth of modern marine analogues—ferruginous conditions continued to locally be a feature of early Phanerozoic seawater .
ArticleNumber 9970
Author Slack, John F
Li, Zhi-Quan
Robbins, Leslie J
Planavsky, Noah J
Xue, Chun-Ji
Zheng, Meng-Tian
Zhang, Lian-Chang
Konhauser, Kurt O
Zhu, Ming-Tian
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Snippet It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history. This view represents a major shift in...
Abstract It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history . This view represents a...
It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history . This view represents a major shift...
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SubjectTerms Geological time
Iron
Marine environment
Sediments
Speciation
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Title Earth's youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean
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Volume 8
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