supported by the National Natural Science Foundation of China(Nos.41802242 and 42174089)。
Paleomagnetic results cannot be applied in global and regional tectonic reconstructions unless the paleosecular variation has been adequately averaged.However,how many sampling sites and samples are enough to calculat...
supported by the National Basic Research Program of China(Grant No.2011CB403003);the College Innovation Research Program of Gansu Province(Grant No.2020B320);the College Innovation Foundation of Gansu Province(Grant No.S202013933013)。
Global climate during the Jurassic has been commonly described as a uniform greenhouse climate for a long time.However,the climate scenario of a cool episode during the Callovian-Oxfordian transition following by a wa...
financially supported by the Strategic Priority Research Program (B type) of the Chinese Academy of Sciences (Grant No. XDB03010404)
Identifying when, where, and how India and Asia collided is a prerequisite to better understand the evolution of the Himalayan-Tibetan Plateau. Whereas with essentially the same published paleomagnetic data, a large r...
The latitudinal richness gradient is a frequent topic of study on the modern landscape,but its history in deep time is much less well known.Here,we preliminarily evaluated the paleolatitudinal richness gradient of vas...