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Orbital-paced Oceanic Anoxic Event 2 evolution and astrochronology in the Mentelle Basin (Australia) at southern high latitudes.

Authors :
Xu, Kang
Zhong, Yi
Tsikos, H.
Chen, Hongjin
Li, Yawei
Source :
Palaeogeography, Palaeoclimatology, Palaeoecology. Sep2024, Vol. 650, pN.PAG-N.PAG. 1p.
Publication Year :
2024

Abstract

The Oceanic Anoxic Event 2 (OAE 2) is widely regarded as one of the most significant global-scale biological and environmental perturbations in the Mesozoic Era. However, the duration and driving mechanisms of this event at southern high latitudes remain largely unknown due to a lack of available geological records. Here, we present a cyclostratigraphic analysis of high-resolution records of lightness variability (L*) and gamma-ray attenuation (GRA) bulk density, which are associated with changes of marine primary productivity and continental weathering, respectively, from Site U1516 located in the Mentelle Basin, offshore southwest Australia. This analysis permits establishment of an astronomical time framework for a stratigraphic interval of 455.205–485.24 m rCCSF (revised Core Composite Depth below Sea Floor) by tuning the 100 kyr filter to short eccentricity. The studied section encompasses the entire OAE 2 interval at the depth of 460.13–473.94 m rCCSF. Based on the established high-resolution astronomical time scale using astronomical tuning of L* records to the short eccentricity cycles (100 kyr), the duration of OAE 2 is estimated to be ∼990 kyr at Site U1516. A relatively high amplitude of short eccentricity occurred at the build-up stage, accompanied by a gradual rise in obliquity amplitude during the recovery phase of the OAE 2. Combining previous proposals for enhanced oceanic water stratification and terrestrial weathering, we suggest that obliquity, coupled with short eccentricity, paced the evolution of this event at southern high latitudes by controlling insolation changes received by the Earth's surface. • The OAE 2 duration is ∼990 kyr at southern high latitudes. • Short orbital eccentricity amplified the large igneous province affection at the OAE 2 build-up stage. • The orbital obliquity paced the OAE 2 recovery stage at southern high latitudes. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00310182
Volume :
650
Database :
Academic Search Index
Journal :
Palaeogeography, Palaeoclimatology, Palaeoecology
Publication Type :
Academic Journal
Accession number :
178857999
Full Text :
https://doi.org/10.1016/j.palaeo.2024.112346