DINOWEB - dinosaurs web-site  

Complete Data Base of Paleozoic and Mesozoic Tetrapods.
Paleo-News and illustrations. Big electronic PDF-library.

line decor
line decor

Download PDF Paleolibrary


?????????? ?????????
сайт о динозаврах
??????? ?????????

рейтинг сайтов
Free Hit Counters

Free Counter
hit counter javascript

myspace hit counter
Powered by counter.bloke.com

Locations of visitors to this page


Obliquity-forced climate during the Early Triassic hothouse in China.

June 30 , 2016

The start of the Mesozoic Era is marked by roughly 5 m.y. of Earth system upheavals, including unstable biotic recovery, repeated global warming, ocean anoxia, and perturbations in the global carbon cycle. Intervals between crises were comparably hospitable to life. The causes of these upheavals are unknown, but are thought to be linked to recurrent Siberian volcanism. Here, two marine sedimentary successions at Chaohu and Daxiakou (South China) are evaluated for paleoclimate change from astronomical forcing. In these sections, gamma-ray variations indicative of terrestrial weathering reveal enhanced obliquity cycling over prolonged intervals, characterized by a 32.8 k.y. periodicity with strong 1.2 m.y. modulations. These suggest a 22 h length of day and 1.2 m.y. interaction between the orbital inclinations of Earth and Mars. Comparing the 1.2 m.y. obliquity modulation cycles in these sections with Early Triassic records of global sea level, temperature, redox, and biotic evolution suggests that long-term astronomical forcing was involved in the repeated climatic and biotic upheavals that took place throughout the Early Triassic.

Mingsong Li, Chunju Huang, Linda Hinnov, James Ogg, Zhong-Qiang Chen, and Yang Zhang (2016)
Obliquity-forced climate during the Early Triassic hothouse in China.
Geology (advance online publication)



Hosted by uCoz