Decoupled δ13Ccarb and δ13Corg records at Triassic–Jurassic boundary interval in eastern Tethys: Environmental implications for spatially different global response
Author:
Funder
Khalifa University of Science, Technology and Research
Petroleum Institute
Publisher
Elsevier BV
Subject
General Earth and Planetary Sciences
Reference78 articles.
1. The Triassic-Jurassic boundary event from an equatorial carbonate platform (Ghalilah Formation, United Arab Emirates);Al-Suwaidi;J. Geol. Soc. Lond.,2016
2. How quick was marine recovery after the end-Triassic mass extinction and what role did anoxia play?;Atkinson;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2019
3. Modelling the impact of pulsed CAMP volcanism on pCO2 and δ13C across the Triassic-Jurassic transition;Bachan;Geol. Mag.,2016
4. Carbon cycle dynamics following the end-Triassic mass extinction: constraints from paired δ13Ccarb and δ13Corg records;Bachan;Geochem. Geophys. Geosyst.,2012
5. The end-Triassic negative δ13C excursion: a lithologic test;Bachan;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2014
Cited by 2 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. Patterns of extinction and recovery across the Triassic–Jurassic boundary interval in three resilient Southern Tethyan carbonate platforms;Palaeogeography, Palaeoclimatology, Palaeoecology;2024-09
2. Mid-Norian to Hettangian record and time-specific oolites during the end-Triassic Mass Extinction at Wadi Milaha, Musandam Peninsula, United Arab Emirates;Journal of Asian Earth Sciences: X;2023-06
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