Helium, inorganic and organic carbon isotopes of fluids and gases across the Costa Rica convergent margin

Scientific data - Tập 6 Số 1
Peter H. Barry1, Mayuko Nakagawa2, Donato Giovannelli2, J. Maarten de Moor3, Matthew O. Schrenk4, Alan Seltzer1, Elena Manini5, Daniele Fattorini6, Marta Di Carlo6, Francesco Regoli6, Katherine Fullerton7, Karen G. Lloyd7
1Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA
2Earth-Life Science Institute, Tokyo Institute for Technology, Tokyo, Japan
3Observatorio Volcanológico y Sismológico de Costa Rica (OVSICORI), Universidad Nacional, Heredia, Costa Rica
4Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, USA
5Institute for Marine Biological and Biotechnological Resources, National Research Council of Italy, CNR-ISMAR, Ancona, Italy
6Dipartimento di Scienze della Vita e dell’Ambiente (DISVA), Università Politecnica delle Marche (UNIVPM), Ancona, Italy
7Department of Microbiology, University of Tennessee, Knoxville, TN, USA

Tóm tắt

Abstract

In 2017, fluid and gas samples were collected across the Costa Rican Arc. He and Ne isotopes, C isotopes as well as total organic and inorganic carbon concentrations were measured. The samples (n = 24) from 2017 are accompanied by (n = 17) samples collected in 2008, 2010 and 2012. He-isotopes ranged from arc-like (6.8 RA) to crustal (0.5 RA). Measured dissolved inorganic carbon (DIC) δ13CVPDB values varied from 3.55 to −21.57‰, with dissolved organic carbon (DOC) following the trends of DIC. Gas phase CO2 only occurs within ~20 km of the arc; δ13CVPDB values varied from −0.84 to −5.23‰. Onsite, pH, conductivity, temperature and dissolved oxygen (DO) were measured; pH ranged from 0.9–10.0, conductivity from 200–91,900 μS/cm, temperatures from 23–89 °C and DO from 2–84%. Data were used to develop a model which suggests that ~91 ± 4.0% of carbon released from the slab/mantle beneath the Costa Rican forearc is sequestered within the crust by calcite deposition with an additional 3.3 ± 1.3% incorporated into autotrophic biomass.

Từ khóa


Tài liệu tham khảo

Barry, P. H. et al. Forearc carbon sequestration reduces long-term volatile recycling into the mantle. Nature 568, 487–492 (2019).

Kelemen, P. B. & Manning, C. E. Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up. Proceedings of the National Academy of Sciences 112, E3997–E4006 (2015).

Shaw, A. M., Hilton, D. R., Fischer, T. P., Walker, J. A. & Alvarado, G. E. Contrasting He–C relationships in Nicaragua and Costa Rica: insights into C cycling through subduction zones. Earth and Planetary Science Letters 214, 499–513 (2003).

Füri, E. et al. Carbon release from submarine seeps at the Costa Rica fore arc: implications for the volatile cycle at the Central America convergent margin. Geochem., Geophys, Geosyst, 11 Q04S21 (2010).

Schwarzenbach, E. M., Früh-Green, G. L., Bernasconi, S. M., Alt, J. C. & Plas, A. Serpentinization and carbon sequestration: A study of two ancient peridotite-hosted hydrothermal systems. Chemical Geology 351, 115–133 (2013).

McCollom, T. M. & Seewald, J. S. Serpentinites, hydrogen, and life. Elements 9, 129–134 (2013).

Hilton, D. R., Fischer, T. P. & Marty, B. Noble gases and volatile recycling at subduction zones. Reviews in mineralogy and geochemistry 47, 319–370 (2002).

Kulongoski, J. T. & Hilton, D. R. A quadrupole‐based mass spectrometric system for the determination of noble gas abundances in fluids. Geochemistry, Geophysics, Geosystems 3, 1–10 (2002).

Füri, E. et al. Apparent decoupling of the He and Ne isotope systematics of the Icelandic mantle: the role of He depletion, melt mixing, degassing fractionation and air interaction. Geochim. Cosmochim. Acta 74, 3307–3332 (2010).

Barry, P. H., Hilton, D. R., Fischer, T. P., De Moor, J. M., Mangasini, F. & Ramirez, C. Helium and carbon isotope systematics of cold “mazuku” CO2 vents and hydrothermal gases and fluids from Rungwe Volcanic Province, southern Tanzania. Chemical Geology 339, 141–156 (2013).

Hilton, D. R. et al. Monitoring of temporal and spatial variations in fumarole helium and carbon dioxide characteristics at Poás and Turrialba volcanoes, Costa Rica (2001–2009). Geochemical Journal 44, 431–440 (2010).

Barry, P. H., Hilton, D. R., Füri, E., Halldórsson, S. A. & Grönvold, K. Carbon isotope and abundance systematics, and CO2 fluxes from Icelandic geothermal gases, fluids and subglacial basalts. Geochim. Cosmochim. Acta 134, 74–99 (2014).

Barry, P. H. et al. Noble gases solubility models of hydrocarbon charge mechanism in the Sleipner Vest gas field. Geochim. Cosmochim. Acta 194, 291–309 (2016).

Braun, S. et al. Cellular content of biomolecules in sub-seafloor microbial communities. Geochim. Cosmochim. Acta 188, 330–351 (2016).

Giovannelli, D. et al. Diversity and distribution of prokaryotes within a shallow-water pockmark field. Front. Microbiol. https://doi.org/10.3389/fmicb.2016.00941 (2016).

Giovannelli, D. et al. Diversity and distribution of prokaryotes within a shallow-water pockmark field. Frontiers in microbiology 941. (2016).

Barry, P. Carbon and noble gas data from Costa Rica seeps, Version 1.0. Interdisciplinary Earth Data Alliance, https://doi.org/10.1594/IEDA/111271 (2019).

Ozima, M. & Podosek, F. A. Noble Gas Geochemistry (Cambridge Univ. Press, 2002).

Hilton, D. R. The helium and carbon isotope systematics of a continental geothermal system: results from monitoring studies at Long Valley caldera (California, U.S.A.). Chem. Geol. 127, 269–295 (1996)..