Oceanic Pasts, Planetary Futures: Deep-Sea Core Data and Temporal Negotiation in the CLIMAP Project (1971–1982)

This article explores the temporalities of deep-sea core research in the 1970s and traces how this small scientific field became a site in which geological, environmental, and political times were negotiated in novel ways. Rather than conceiving of deep-sea cores as containers of data, which provide unmediated access to the planetary past, the article shows how the cores were temporally fluid objects which, in the 1970s, were picked up in settings well beyond the ocean sciences. By following the evolution of the deep-sea core project Climate: Long range Investigation, Mapping, and Prediction (CLIMAP), which brought together deep-sea core research with climate modeling and economic and agricultural forecasting, the article argues that the ways in which deep-sea core data entered the field of climate modeling mirrored contemporary fears of overpopulation as well as dreams of abundant energy reserves hidden in the seabed. Even though the deep-sea core scientists spoke of their work as “exploration” or “discovery,” the history of CLIMAP reveals a much more temporally complex enterprise and highlights the instability of planetary and historical times in the postwar era. Drawing on recent developments in time studies as well as the history of the geosciences, the article shows how present theoretical deliberations on the temporalities of the planetary scale can be understood in light of a longer historical process of negotiating multiple temporalities in the geosciences. By considering the history of deep-sea core research in the 1970s as a history of temporal negotiation, the article calls for increased collaboration and engagement between time studies and the history of science.

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Publication Details

Journal
Time & Society
Published
2025-02-13
DOI
https://doi.org/10.1177/0961463x251313854
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Oceanic Pasts, Planetary Futures: Deep-Sea Core Data and Temporal Negotiation in the CLIMAP Project (1971–1982)

Erik Isberg
Time & Society
Geology and Paleoclimatology Research
article

Oceanic Pasts, Planetary Futures: Deep-Sea Core Data and Temporal Negotiation in the CLIMAP Project (1971–1982)

Erik Isberg
article en

Abstract

This article explores the temporalities of deep-sea core research in the 1970s and traces how this small scientific field became a site in which geological, environmental, and political times were negotiated in novel ways. Rather than conceiving of deep-sea cores as containers of data, which provide unmediated access to the planetary past, the article shows how the cores were temporally fluid objects which, in the 1970s, were picked up in settings well beyond the ocean sciences. By following the evolution of the deep-sea core project Climate: Long range Investigation, Mapping, and Prediction (CLIMAP), which brought together deep-sea core research with climate modeling and economic and agricultural forecasting, the article argues that the ways in which deep-sea core data entered the field of climate modeling mirrored contemporary fears of overpopulation as well as dreams of abundant energy reserves hidden in the seabed. Even though the deep-sea core scientists spoke of their work as “exploration” or “discovery,” the history of CLIMAP reveals a much more temporally complex enterprise and highlights the instability of planetary and historical times in the postwar era. Drawing on recent developments in time studies as well as the history of the geosciences, the article shows how present theoretical deliberations on the temporalities of the planetary scale can be understood in light of a longer historical process of negotiating multiple temporalities in the geosciences. By considering the history of deep-sea core research in the 1970s as a history of temporal negotiation, the article calls for increased collaboration and engagement between time studies and the history of science.

Time & Society
KTH Royal Institute of Technology (SE)
H2020 European Research Council
Openalex Percentile: Top 98%
Geology and Paleoclimatology Research
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