Spatiotemporal variations of sedimentary carbon and nitrogen isotopic compositions in the Yangtze Shelf Sea across the Ordovician-Silurian boundary

The Hirnantian Glaciation resulted in a perturbation in global carbon cycling, which is recognized as a positive excursion in the δ13C values of both carbonates and organic matter. To investigate the factors controlling the carbon and nitrogen cycles from the late Ordovician to the early Silurian, t...

Full description

Saved in:
Bibliographic Details
Published inPalaeogeography, palaeoclimatology, palaeoecology Vol. 567; p. 110257
Main Authors Yang, Xiangrong, Yan, Detian, Chen, Daizhao, Liu, Mu, She, Xiaohui, Zhang, Bao, Zhang, Liwei, Zhang, Junfeng
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.04.2021
Subjects
Online AccessGet full text

Cover

Loading…