Articles | Volume 18, issue 9
https://doi.org/10.5194/cp-18-2117-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-18-2117-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Shallow marine carbonates as recorders of orbitally induced past climate changes – example from the Oxfordian of the Swiss Jura Mountains
André Strasser
CORRESPONDING AUTHOR
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Invited contribution by André Strasser, recipient of the EGU Jean Baptiste Lamarck Medal 2021.
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For a long time, human beings have lived with the idea of cycles, as attested by many ancient traditions. This perception led our way of observing and interpreting the most diverse types of phenomena. In the Earth sciences, cyclicity has crucial epistemological value. It offers simple solutions for cause and consequence analysis in time and space. The intention here is to review how such ideas emerged in the geosciences, supporting current stratigraphic principles and practices.
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For a long time, human beings have lived with the idea of cycles, as attested by many ancient traditions. This perception led our way of observing and interpreting the most diverse types of phenomena. In the Earth sciences, cyclicity has crucial epistemological value. It offers simple solutions for cause and consequence analysis in time and space. The intention here is to review how such ideas emerged in the geosciences, supporting current stratigraphic principles and practices.
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Co-editor-in-chief
The paper presents an interesting review of deep time ecosystems and suggests that the interpretation of the evolution of ancient sedimentary systems can be refined and better compared to today’s changes in ecosystems. Concerning the rate of climate change, this study implies that anthropogenically induced global warming and subsequent sea level rise today occurs more than ten times faster than the fastest rise reconstructed for the Oxfordian (159 Ma - 154 Ma)
The paper presents an interesting review of deep time ecosystems and suggests that the...
Short summary
Some 155 million years ago, sediments were deposited in a shallow subtropical sea. Coral reefs formed in a warm and arid climate during high sea level, and clays were washed into the ocean at low sea level and when it rained. Climate and sea level changes were induced by cyclical insolation changes. Analysing the sedimentary record, it appears that sea level rise today (as a result of global warming) is more than 10 times faster than the fastest rise reconstructed from the geologic past.
Some 155 million years ago, sediments were deposited in a shallow subtropical sea. Coral reefs...
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