A long section of serpentinized depleted mantle peridotite-Reference-Cited by-同舟云学术

A long section of serpentinized depleted mantle peridotite

Published:2024-08-09 Issue:6709 Volume:385 Page:623-629
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Lissenberg C. Johan¹^ORCID,McCaig Andrew M.²^ORCID,Lang Susan Q.³,Blum Peter⁴^ORCID,Abe Natsue⁵^ORCID,Brazelton William J.⁶^ORCID,Coltat Rémi⁷^ORCID,Deans Jeremy R.⁸^ORCID,Dickerson Kristin L.⁹^ORCID,Godard Marguerite¹⁰^ORCID,John Barbara E.¹¹,Klein Frieder¹²^ORCID,Kuehn Rebecca¹³^ORCID,Lin Kuan-Yu¹⁴^ORCID,Liu Haiyang¹⁵^ORCID,Lopes Ethan L.¹⁶^ORCID,Nozaka Toshio¹⁷^ORCID,Parsons Andrew J.¹⁸^ORCID,Pathak Vamdev¹⁹^ORCID,Reagan Mark K.²⁰^ORCID,Robare Jordyn A.²¹^ORCID,Savov Ivan P.²^ORCID,Schwarzenbach Esther M.²²^ORCID,Sissmann Olivier J.²³^ORCID,Southam Gordon²⁴^ORCID,Wang Fengping²⁵^ORCID,Wheat C. Geoffrey²⁶^ORCID,Anderson Lesley²⁷,Treadwell Sarah²⁸²⁹

Affiliation:

1. School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK.

2. School of Earth and Environment, University of Leeds, Leeds, UK.

3. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.

4. International Ocean Discovery Program, Texas A&M University, College Station, TX, USA.

5. Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan.

6. School of Biological Sciences, University of Utah, Salt Lake City, UT, USA.

7. Instituto Andaluz de Ciencias de la Tierra, CSIC-UGR, Granada, Spain.

8. School of Biological, Environmental, and Earth Sciences, University of Southern Mississippi, Hattiesburg, MS, USA.

9. Department of Earth and Planetary Sciences, University of California, Santa Cruz, Santa Cruz, CA, USA.

10. Geosciences Montpellier, CNRS, University of Montpellier, Montpellier, France.

11. Department of Geology and Geophysics, University of Wyoming, Laramie, WY, USA.

12. Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.

13. Institute of Geosciences and Geography, Martin-Luther-University Halle-Wittenberg, Halle, Germany.

14. Department of Earth Sciences, University of Delaware, Newark, DE, USA.

15. Center of Deep Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China.

16. Department of Geophysics, Stanford University, Stanford, CA, USA.

17. Department of Earth Sciences, Okayama University, Okayama, Japan.

18. School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.

19. Department of Geology, Central University of Punjab, Bathinda, India.

20. Department of Earth and Environmental Sciences, University of Iowa, Iowa City, IA, USA.

21. School of Molecular Sciences, Arizona State University, Phoenix, AZ, USA.

22. Department of Geosciences, University of Fribourg, Fribourg, Switzerland.

23. IFP Energies Nouvelles, Paris, France.

24. School of the Environment, The University of Queensland, St. Lucia, QLD, Australia.

25. Key Laboratory of Polar Ecosystem and Climate Change, Ministry of Education; and School of Oceanography, Shanghai Jiao Tong University, Shanghai 200030, China.

26. Global Undersea Research Unit, University of Alaska Fairbanks, Moss Landing, CA, USA.

27. Arctic Research Support and Logistics, Washington, DC, USA.

28. Department of Communication, University of North Dakota, Grand Forks, ND, USA.

29. Blue Marble Space Institute of Science, Seattle, WA, USA.

Abstract

The upper mantle is critical for our understanding of terrestrial magmatism, crust formation, and element cycling between Earth’s solid interior, hydrosphere, atmosphere, and biosphere. Mantle composition and evolution have been primarily inferred by surface sampling and indirect methods. We recovered a long (1268-meter) section of serpentinized abyssal mantle peridotite interleaved with thin gabbroic intrusions. We find depleted compositions with notable variations in mantle mineralogy controlled by melt flow. Dunite zones have predominantly intermediate dips, in contrast to the originally steep mantle fabrics, indicative of oblique melt transport. Extensive hydrothermal fluid-rock interaction is recorded across the full depth of the core and is overprinted by oxidation in the upper 200 meters. Alteration patterns are consistent with vent fluid composition in the nearby Lost City hydrothermal field.

Publisher

American Association for the Advancement of Science (AAAS)

Link

https://www.science.org/doi/pdf/10.1126/science.adp1058

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