Barium isotopes in stromatolites through deep-time: A novel tracer for metal cycling in the photic zone

authored by

Simon V. Hohl, Yi-Bo Lin, Hai-Zhen Wei, Guany-Yi Wei, Sebastian Viehmann

Abstract

In the search for reliable archives to reconstruct Earth's paleo-surface ocean chemistry, stromatolites have gained much attention in the past decade. Stromatolitic carbonates, i.e., lithified microbial mats, form in shallow neritic environments and have the unique potential to record the ambient water chemistry of the photic zone. Their wide occurrence in shallow marine sedimentary successions from at least ca. 3.5 billion years ago until today highlight these bio-sedimentary archives as excellent recorders of elemental fluctuations in microbial habitats of the near-shore surface ocean, embayed basins, and lacustrine systems. In this study, we test the application of Ba concentrations and its isotopes in Paleoarchean to Holocene stromatolites as a potential deep-time proxy for biogeochemical element cycling in ancient microbial habitats of different depositional environments. Barium systematics in stromatolites reflect biogeochemical Ba cycling in local, aqueous (micro)environments of photic zones under variable oxygen and sulphate saturation conditions. We obtained significant differences in authigenic Ba concentrations and isotopic compositions between open ocean and restricted depositional settings: Microbial communities in restricted embayment or lacustrine environments show distinct negative δ

¹³⁸Ba

_auth values inversely correlated with Ba concentrations due to Ba (re)cycling. In contrast, stromatolites from non-restricted, marine depositional settings have the potential to record ambient seawater Ba isotopic compositions with the heaviest obtained δ

¹³⁸Ba

_sw = 0.45 ‰ in the Archean, 0.61 ‰ in the Proterozoic and 0.57 ‰ in the Phanerozoic at a precision of ±0.04 ‰ (2SD). Our study suggests that variabilities in δ

¹³⁸Ba of stromatolitic carbonates can directly be linked to environmental restriction and associated biogeochemical Ba cycling, probably related to micro-barite formation on microbial biofilms, with subsequent recycling in restricted environments leading to lighter Ba isotopic values in the ambient waters and carbonates. However, stromatolites of open marine settings record local surface ocean δ

¹³⁸Ba compositions and may be used as unique archives in future studies to investigate the evolution of primary productivity in the photic zone through deep-time.

Organisation(s)

Institute of Mineralogy
Geochemistry

External Organisation(s)

Tongji University
State Key Laboratory of Marine Geology
Nanjing University

Type

Article

Journal

Earth and Planetary Science Letters

Volume

632

ISSN

0012-821X

Publication date

15.04.2024

Publication status

Published

Peer reviewed

Yes

ASJC Scopus subject areas

Geochemistry and Petrology, Geophysics, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous)

Sustainable Development Goals

SDG 14 - Life Below Water

Electronic version(s)

https://doi.org/10.1016/j.epsl.2024.118639 (Access: Closed)