Towards a stable astronomical time scale for the Paleocene: Aligning Shatsky Rise with the Zumaia – Walvis Ridge ODP Site 1262 composite

2015 ◽  
Vol 48 (1) ◽  
pp. 91-110 ◽  
Author(s):  
Frederik J. Hilgen ◽  
Hemmo A. Abels ◽  
Klaudia F. Kuiper ◽  
Lucas J. Lourens ◽  
Mariëtte Wolthers
Science ◽  
2019 ◽  
Vol 365 (6456) ◽  
pp. 926-929 ◽  
Author(s):  
Richard E. Zeebe ◽  
Lucas J. Lourens

Astronomical calculations reveal the Solar System’s dynamical evolution, including its chaoticity, and represent the backbone of cyclostratigraphy and astrochronology. An absolute, fully calibrated astronomical time scale has hitherto been hampered beyond ~50 million years before the present (Ma) because orbital calculations disagree before that age. Here, we present geologic data and a new astronomical solution (ZB18a) showing exceptional agreement from ~58 to 53 Ma. We provide a new absolute astrochronology up to 58 Ma and a new Paleocene–Eocene boundary age (56.01 ± 0.05 Ma). We show that the Paleocene–Eocene Thermal Maximum (PETM) onset occurred near a 405-thousand-year (kyr) eccentricity maximum, suggesting an orbital trigger. We also provide an independent PETM duration (170 ± 30 kyr) from onset to recovery inflection. Our astronomical solution requires a chaotic resonance transition at ~50 Ma in the Solar System’s fundamental frequencies.


2015 ◽  
Vol 11 (3) ◽  
pp. 1665-1699 ◽  
Author(s):  
T. Westerhold ◽  
U. Röhl ◽  
T. Frederichs ◽  
S. M. Bohaty ◽  
J. C. Zachos

Abstract. To explore cause and consequences in past climate reconstructions highly accuracy age models are inevitable. The highly accurate astronomical calibration of the geological time scale beyond 40 million years critically depends on the accuracy of orbital models and radio-isotopic dating techniques. Discrepancies in the age dating of sedimentary successions and the lack of suitable records spanning the middle Eocene have prevented development of a continuous astronomically calibrated geological timescale for the entire Cenozoic Era. We now solve this problem by constructing an independent astrochronological stratigraphy based on Earth's stable 405 kyr eccentricity cycle between 41 and 48 million years ago (Ma) with new data from deep-sea sedimentary sequences in the South Atlantic Ocean. This new link completes the Paleogene astronomical time scale and confirms the intercalibration of radio-isotopic and astronomical dating methods back through the Paleocene-Eocene Thermal Maximum (PETM, 55.930 Ma) and the Cretaceous/Paleogene boundary (66.022 Ma). Coupling of the Paleogene 405 kyr cyclostratigraphic frameworks across the middle Eocene further paves the way for extending the Astronomical Time Scale (ATS) into the Mesozoic.


Author(s):  
A. Berger ◽  
TH. Fichefet ◽  
H. Gallee ◽  
I. Marsiat ◽  
CH. Tricot ◽  
...  

2018 ◽  
Vol 63 (22) ◽  
pp. 1485-1494 ◽  
Author(s):  
Yu Sui ◽  
Chunju Huang ◽  
Rui Zhang ◽  
Zhixiang Wang ◽  
James Ogg ◽  
...  

2019 ◽  
Vol 532 ◽  
pp. 109253 ◽  
Author(s):  
Ke Xu ◽  
Honghan Chen ◽  
Chunju Huang ◽  
James G. Ogg ◽  
Jingxiu Zhu ◽  
...  

Geology ◽  
2018 ◽  
Vol 47 (1) ◽  
pp. 83-86 ◽  
Author(s):  
Huaichun Wu ◽  
Qiang Fang ◽  
Xiangdong Wang ◽  
Linda A. Hinnov ◽  
Yuping Qi ◽  
...  
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