GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania

Paper No. 129-2
Presentation Time: 1:50 PM

RECONSTRUCTING THE SECULAR EVOLUTION OF LITHIUM ISOTOPE COMPOSITION OF SEAWATER FROM MARINE HALITE


WELDEGHEBRIEL, Mebrahtu, Department of Geosciences, Princeton University, Princeton, NJ 08544, MURPHY, Jack G., Department of Earth & Environmental Science, University of Pennsylvania, Philadelphia, PA 19104, JURIKOVA, Hana, School of Earth and Environmental Sciences, University of St Andrews, St Andrews, KY169TS, United Kingdom, LOWENSTEIN, Tim K., Department of Earth Sciences, Binghamton University, Binghamton, NY 13902-6000, RAE, James, School of Earth & Enviro Sciences, University of St Andrews, St Andrews, KY169AL, United Kingdom, NIESPOLO, Elizabeth, Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709 and HIGGINS, John, The Department of Geosciences, Princeton University, Guyot Hall, Princeton, NJ 08544

The lithium isotopic composition of seawater (δ7LiSW) has emerged as a promising tracer for reconstructing global terrestrial silicate weathering and marine reverse weathering. Both terrestrial chemical weathering and marine reverse weathering are hypothesized to play important roles in regulating Earth’s geologic carbon cycle and climate [1,2]. Testing these hypothesized mechanisms requires establishing accurate records of ancient δ7Lisw. Recent records of δ7Lisw derived from foraminifera [2], brachiopods [3,4], and shallow marine carbonates [5] show an increase of ∼8–9‰ over the past 60 Myr. However, laboratory experiments [6] and studies of drill cores from modern carbonate platforms [7] suggest that reconstructing past seawater δ7Li values from skeletal and non-skeletal carbonates is complicated by vital effects, diagenesis, and mineralogy (e.g., calcite vs. aragonite). Thus, other archives are needed to determine whether δ7Li values measured in carbonates indeed reflect secular changes in δ7Lisw. Here, we present lithium isotope ratio measurements of fluid inclusions in marine halites collected from modern salinas (solar evaporation ponds) and large suite of Neoproterozoic and Phanerozoic evaporite basins. These fluid inclusions were previously used to document the major, minor, and trace element composition of paleoseawater, including lithium concentration [8]. Lithium isotope ratios measured in ancient marine halites provide an independent archive of δ7Lisw, extending the record of the δ7Lisw to 550 Myr.

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