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Title: The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record

Abstract

Combining U–Pb ages with Lu–Hf data in zircon provides insights into the magmatic history of rocky planets. The Northwest Africa (NWA) 7034/7533 meteorites are samples of the southern highlands of Mars containing zircon with ages as old as 4476.3 ± 0.9 Ma, interpreted to reflect reworking of the primordial Martian crust by impacts. We extracted a statistically significant zircon population (n= 57) from NWA 7533 that defines a temporal record spanning 4.2 Gyr. Ancient zircons record ages from 4485.5 ± 2.2 Ma to 4331.0 ± 1.4 Ma, defining a bimodal distribution with groupings at 4474 ± 10 Ma and 4442 ± 17 Ma. We interpret these to represent intense bombardment episodes at the planet’s surface, possibly triggered by the early migration of gas giant planets. The unradiogenic initial Hf-isotope composition of these zircons establishes that Mars’s igneous activity prior to ~4.3 Ga was limited to impact-related reworking of a chemically enriched, primordial crust. A group of younger detrital zircons record ages from 1548.0 ± 8.8 Ma to 299.5 ± 0.6 Ma. The only plausible sources for these grains are the temporally associated Elysium and Tharsis volcanic provinces that are the expressions of deep-seated mantle plumes. The chondritic-like Hf-isotope compositions ofmore » these zircons require the existence of a primitive and convecting mantle reservoir, indicating that Mars has been in a stagnant-lid tectonic regime for most of its history. Our results imply that zircon is ubiquitous on the Martian surface, providing a faithful record of the planet’s magmatic history.« less

Authors:
 [1];  [1];  [1];  [1]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [4];  [5]; ORCiD logo [5];  [6];  [7]; ORCiD logo [8];  [8]; ORCiD logo [9]
  1. Univ. of Copenhagen (Denmark)
  2. Univ. of Tokyo (Japan)
  3. British Geological Survey, Nottingham (United Kingdom)
  4. European Synchrotron Radiation Facility (ESRF), Grenoble (France)
  5. Univ. of Paris (France)
  6. Univ. de Bretagne Occidentale (France)
  7. Univ. of Western Australia, Perth, WA (Australia)
  8. Curtin Univ., Perth, WA (Australia)
  9. Univ. of Copenhagen (Denmark); Univ. of Paris (France)
Publication Date:
Research Org.:
Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
Sponsoring Org.:
USDOE Office of Science (SC); Carlsberg Foundation; Danish Research Foundation; European Research Council (ERC); Australian Research Council
OSTI Identifier:
1734929
Grant/Contract Number:  
AC02-06CH11357; CF18_1105; DNRF97; 833275; DP190103849
Resource Type:
Accepted Manuscript
Journal Name:
Proceedings of the National Academy of Sciences of the United States of America
Additional Journal Information:
Journal Volume: 117; Journal Issue: 49; Journal ID: ISSN 0027-8424
Publisher:
National Academy of Sciences
Country of Publication:
United States
Language:
ENGLISH
Subject:
58 GEOSCIENCES; Mars; meteorites; ziricon; geodynamics

Citation Formats

Costa, Maria M., Jensen, Ninna K., Bouvier, Laura C., Connelly, James N., Mikouchi, Takashi, Horstwood, Matthew A., Suuronen, Jussi-Petteri, Moynier, Frédéric, Deng, Zhengbin, Agranier, Arnaud, Martin, Laure J., Johnson, Tim E., Nemchin, Alexander A., and Bizzarro, Martin. The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record. United States: N. p., 2020. Web. doi:10.1073/pnas.2016326117.
Costa, Maria M., Jensen, Ninna K., Bouvier, Laura C., Connelly, James N., Mikouchi, Takashi, Horstwood, Matthew A., Suuronen, Jussi-Petteri, Moynier, Frédéric, Deng, Zhengbin, Agranier, Arnaud, Martin, Laure J., Johnson, Tim E., Nemchin, Alexander A., & Bizzarro, Martin. The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record. United States. https://doi.org/10.1073/pnas.2016326117
Costa, Maria M., Jensen, Ninna K., Bouvier, Laura C., Connelly, James N., Mikouchi, Takashi, Horstwood, Matthew A., Suuronen, Jussi-Petteri, Moynier, Frédéric, Deng, Zhengbin, Agranier, Arnaud, Martin, Laure J., Johnson, Tim E., Nemchin, Alexander A., and Bizzarro, Martin. Mon . "The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record". United States. https://doi.org/10.1073/pnas.2016326117. https://www.osti.gov/servlets/purl/1734929.
@article{osti_1734929,
title = {The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record},
author = {Costa, Maria M. and Jensen, Ninna K. and Bouvier, Laura C. and Connelly, James N. and Mikouchi, Takashi and Horstwood, Matthew A. and Suuronen, Jussi-Petteri and Moynier, Frédéric and Deng, Zhengbin and Agranier, Arnaud and Martin, Laure J. and Johnson, Tim E. and Nemchin, Alexander A. and Bizzarro, Martin},
abstractNote = {Combining U–Pb ages with Lu–Hf data in zircon provides insights into the magmatic history of rocky planets. The Northwest Africa (NWA) 7034/7533 meteorites are samples of the southern highlands of Mars containing zircon with ages as old as 4476.3 ± 0.9 Ma, interpreted to reflect reworking of the primordial Martian crust by impacts. We extracted a statistically significant zircon population (n= 57) from NWA 7533 that defines a temporal record spanning 4.2 Gyr. Ancient zircons record ages from 4485.5 ± 2.2 Ma to 4331.0 ± 1.4 Ma, defining a bimodal distribution with groupings at 4474 ± 10 Ma and 4442 ± 17 Ma. We interpret these to represent intense bombardment episodes at the planet’s surface, possibly triggered by the early migration of gas giant planets. The unradiogenic initial Hf-isotope composition of these zircons establishes that Mars’s igneous activity prior to ~4.3 Ga was limited to impact-related reworking of a chemically enriched, primordial crust. A group of younger detrital zircons record ages from 1548.0 ± 8.8 Ma to 299.5 ± 0.6 Ma. The only plausible sources for these grains are the temporally associated Elysium and Tharsis volcanic provinces that are the expressions of deep-seated mantle plumes. The chondritic-like Hf-isotope compositions of these zircons require the existence of a primitive and convecting mantle reservoir, indicating that Mars has been in a stagnant-lid tectonic regime for most of its history. Our results imply that zircon is ubiquitous on the Martian surface, providing a faithful record of the planet’s magmatic history.},
doi = {10.1073/pnas.2016326117},
journal = {Proceedings of the National Academy of Sciences of the United States of America},
number = 49,
volume = 117,
place = {United States},
year = {Mon Nov 16 00:00:00 EST 2020},
month = {Mon Nov 16 00:00:00 EST 2020}
}

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