Tracking δ13C and δ18O fluctuations uncovers stable modes and key patterns of paleoclimate

The examination of fluctuations in the correlations between δ13C and δ18O is of significant importance for the reconstruction of the Earth’s climate history. A key challenge in paleoclimatology is finding a suitable method to represent the correlated fluctuation system between δ13C and δ18O. The met...

Full description

Bibliographic Details
Main Authors: Shifeng Sun, Haiying Wang, Yongjian Huang
Format: Article
Language:English
Published: Elsevier 2024-07-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S167498712400029X