Peridotite weathering is the missing ingredient of Earth's continental crust composition

Andreas Beinlich, Håkon Austrheim, Vasileios Mavromatis, Ben Grguric, Christine V. Putnis, Andrew Putnis

Research output: Contribution to journalArticleResearchpeer-review

Abstract

The chemical composition of the continental crust cannot be adequately explained by current models for its formation, because it is too rich in Ni and Cr compared to that which can be generated by any of the proposed mechanisms. Estimates of the crust composition are derived from average sediment, while crustal growth is ascribed to amalgamation of differentiated magmatic rocks at continental margins. Here we show that chemical weathering of Ni- and Cr-rich, undifferentiated ultramafic rock equivalent to ~1.3 wt% of today's continental crust compensates for low Ni and Cr in formation models of the continental crust. Ultramafic rock weathering produces a residual that is enriched in Ni and also silica. In the light of potentially large volumes of ultramafic rock and high atmospheric CO2 concentrations during the Archean, chemical weathering must therefore have played a major role in forming compositionally evolved components of the early Earth's crust.

Original languageEnglish
Article number634
JournalNature Communications
Volume9
Issue number1
DOIs
Publication statusPublished - 1 Dec 2018
Externally publishedYes

Fingerprint

peridotite
weathering
Weathering
ingredients
Silicon Dioxide
crusts
Earth (planet)
Rocks
rocks
Growth
Chemical analysis
Earth crust
continental shelves
Sediments
chemical composition
sediments
silicon dioxide
estimates

ASJC Scopus subject areas

  • Chemistry(all)
  • Biochemistry, Genetics and Molecular Biology(all)
  • Physics and Astronomy(all)

Cite this

Peridotite weathering is the missing ingredient of Earth's continental crust composition. / Beinlich, Andreas; Austrheim, Håkon; Mavromatis, Vasileios; Grguric, Ben; Putnis, Christine V.; Putnis, Andrew.

In: Nature Communications, Vol. 9, No. 1, 634, 01.12.2018.

Research output: Contribution to journalArticleResearchpeer-review

Beinlich, Andreas ; Austrheim, Håkon ; Mavromatis, Vasileios ; Grguric, Ben ; Putnis, Christine V. ; Putnis, Andrew. / Peridotite weathering is the missing ingredient of Earth's continental crust composition. In: Nature Communications. 2018 ; Vol. 9, No. 1.
@article{d339d0d4ea674cbd93e614eea77e3255,
title = "Peridotite weathering is the missing ingredient of Earth's continental crust composition",
abstract = "The chemical composition of the continental crust cannot be adequately explained by current models for its formation, because it is too rich in Ni and Cr compared to that which can be generated by any of the proposed mechanisms. Estimates of the crust composition are derived from average sediment, while crustal growth is ascribed to amalgamation of differentiated magmatic rocks at continental margins. Here we show that chemical weathering of Ni- and Cr-rich, undifferentiated ultramafic rock equivalent to ~1.3 wt{\%} of today's continental crust compensates for low Ni and Cr in formation models of the continental crust. Ultramafic rock weathering produces a residual that is enriched in Ni and also silica. In the light of potentially large volumes of ultramafic rock and high atmospheric CO2 concentrations during the Archean, chemical weathering must therefore have played a major role in forming compositionally evolved components of the early Earth's crust.",
author = "Andreas Beinlich and H{\aa}kon Austrheim and Vasileios Mavromatis and Ben Grguric and Putnis, {Christine V.} and Andrew Putnis",
year = "2018",
month = "12",
day = "1",
doi = "10.1038/s41467-018-03039-9",
language = "English",
volume = "9",
journal = "Nature Communications",
issn = "2041-1723",
publisher = "Nature Publishing Group",
number = "1",

}

TY - JOUR

T1 - Peridotite weathering is the missing ingredient of Earth's continental crust composition

AU - Beinlich, Andreas

AU - Austrheim, Håkon

AU - Mavromatis, Vasileios

AU - Grguric, Ben

AU - Putnis, Christine V.

AU - Putnis, Andrew

PY - 2018/12/1

Y1 - 2018/12/1

N2 - The chemical composition of the continental crust cannot be adequately explained by current models for its formation, because it is too rich in Ni and Cr compared to that which can be generated by any of the proposed mechanisms. Estimates of the crust composition are derived from average sediment, while crustal growth is ascribed to amalgamation of differentiated magmatic rocks at continental margins. Here we show that chemical weathering of Ni- and Cr-rich, undifferentiated ultramafic rock equivalent to ~1.3 wt% of today's continental crust compensates for low Ni and Cr in formation models of the continental crust. Ultramafic rock weathering produces a residual that is enriched in Ni and also silica. In the light of potentially large volumes of ultramafic rock and high atmospheric CO2 concentrations during the Archean, chemical weathering must therefore have played a major role in forming compositionally evolved components of the early Earth's crust.

AB - The chemical composition of the continental crust cannot be adequately explained by current models for its formation, because it is too rich in Ni and Cr compared to that which can be generated by any of the proposed mechanisms. Estimates of the crust composition are derived from average sediment, while crustal growth is ascribed to amalgamation of differentiated magmatic rocks at continental margins. Here we show that chemical weathering of Ni- and Cr-rich, undifferentiated ultramafic rock equivalent to ~1.3 wt% of today's continental crust compensates for low Ni and Cr in formation models of the continental crust. Ultramafic rock weathering produces a residual that is enriched in Ni and also silica. In the light of potentially large volumes of ultramafic rock and high atmospheric CO2 concentrations during the Archean, chemical weathering must therefore have played a major role in forming compositionally evolved components of the early Earth's crust.

UR - http://www.scopus.com/inward/record.url?scp=85042008632&partnerID=8YFLogxK

U2 - 10.1038/s41467-018-03039-9

DO - 10.1038/s41467-018-03039-9

M3 - Article

VL - 9

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

IS - 1

M1 - 634

ER -