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

Xu, Kang1; Zhong, Yi2; Tsikos, H.3; Chen, Hongjin4; Li, Yawei1

2024-09-15

10.1016/j.palaeo.2024.112346

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY   影响因子和分区

0031-0182

1872-616X

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.

Oceanic Anoxic Event 2 (OAE 2) Southern high latitudes Lightness variability Gamma-ray attenuation bulk density Astrochronology

SCI

英语

其他

National Natural Science Foundation of China["42274094","42306089"] ; State Key Laboratory of Marine Geology, Tongji University[MGK202209] ; Talent Promotion Project of Pingdingshan University["PXY-BSQD-2022036","PXY-BSQD-2022035"]

Physical Geography ; Geology ; Paleontology

Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology

WOS:001264829300001

ELSEVIER

GEOSCIENCES

Web of Science

1.Pingdingshan Univ, Sch Tourism & Planning, Pingdingshan 467000, Henan, Peoples R China
2.Southern Univ Sci & Technol, Ctr Marine Magnetism, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China
3.Univ Patras, Dept Geol, GR-26504 Rion, Greece
4.China Geol Survey, Minist Nat Resources, Guangzhou Marine Geol Survey, Key Lab Marine Mineral Resources, Guangzhou 510075, Peoples R China

Xu, Kang,Zhong, Yi,Tsikos, H.,et al. Orbital-paced Oceanic Anoxic Event 2 evolution and astrochronology in the Mentelle Basin (Australia) at southern high latitudes[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2024,650.

Xu, Kang,Zhong, Yi,Tsikos, H.,Chen, Hongjin,&Li, Yawei.(2024).Orbital-paced Oceanic Anoxic Event 2 evolution and astrochronology in the Mentelle Basin (Australia) at southern high latitudes.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,650.

Xu, Kang,et al."Orbital-paced Oceanic Anoxic Event 2 evolution and astrochronology in the Mentelle Basin (Australia) at southern high latitudes".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 650(2024).