Climate changes as recorded in stable carbon isotopic compositions of the Late Jurassic marine sedimentary succession in the Qiangtang Basin, Northern Tibet

Author(s)
Gaojie Li, Guoqing Xia, Haisheng Yi, Chihua Wu, Michael Wagreich
Abstract

The Jurassic oceanographic and climatic evolution is considered to be related to the breakup of Pangaea. As a crucial component of the carbon cycle, atmospheric CO

2 concentration (pCO

2) has been postulated as a main driver for climate change during the Jurassic, and concomitant changes in paleo-oceanographic conditions occurred as a result. In this study, we present a high-resolution organic matter (kerogen) carbon isotope dataset (δ

13C

kerogen) from Upper Jurassic marine sedimentary rocks in the Qiangtang Basin, Tibet. The δ

13C

kerogen result contains a genuine record concerning the response of the eastern Tethys to exogenic carbon cycle perturbations in both marine and atmospheric reservoirs and is also consistent with the high-resolution bulk carbonate and organic matter carbon-isotope records from the Atlantic and western Tethys. The relative fractionation of carbon isotopes in organic matter vs. carbonate species, defined as Δ

13C (δ

13C

carb

13C

kerogen), and the secular trend of atmospheric pCO

2 over the Late Jurassic that is calculated from the high-resolution δ

13C

kerogen values indicate a cold Callovian-Oxfordian transition, a long-term increasing but fluctuating Kimmeridgian and a prominent early Tithonian cooling event (ETCE). The pronounced temperature plateau during the late Kimmeridgian-early Tithonian was contemporaneous with the occurrence of major magmatic events during the Late Jurassic, while the ETCE has been possibly attributed to major changes in oceanic circulation patterns. Additionally, reconstructed atmospheric pCO

2 values show very small differences to values using phytane- and stomatal density-based pCO

2 calculations, providing an alternative estimate for accurate identification of the paleoclimatic framework of this enigmatic interval in the Mesozoic.

Organisation(s)
Department of Geology
External organisation(s)
Mianyang Teachers' College, Chengdu University of Technology, Southwest Petroleum University
Journal
Journal of Asian Earth Sciences
Volume
236
No. of pages
13
ISSN
1367-9120
DOI
https://doi.org/10.1016/j.jseaes.2022.105317
Publication date
09-2022
Peer reviewed
Yes
Austrian Fields of Science 2012
105105 Geochemistry, 105123 Stratigraphy
Keywords
ASJC Scopus subject areas
Earth-Surface Processes, Geology
Sustainable Development Goals
SDG 14 - Life Below Water, SDG 13 - Climate Action
Portal url
https://ucris.univie.ac.at/portal/en/publications/climate-changes-as-recorded-in-stable-carbon-isotopic-compositions-of-the-late-jurassic-marine-sedimentary-succession-in-the-qiangtang-basin-northern-tibet(320bc8c8-0f86-48eb-8e2c-84707e5025cd).html