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Limited freshwater cap in the Eocene Arctic Ocean
Lisa A Neville1,2, Stephen E Grasby3, David H McNeil1
1Geological Survey of Canada, Natural Resources Canada, Calgary, Alberta, T2L 2A7, Canada.
The Eocene Arctic Ocean may not have had widespread freshwater caps. New evidence suggests Azolla events were linked to increased river runoff, not global freshwater layers, impacting climate models.
Area of Science:
- Paleoceanography
- Paleoclimatology
- Geology
Background:
- Eocene (~50 Ma ago) Arctic Ocean sediment records, specifically Azolla fern remains on the Lomonosov Ridge, previously suggested widespread seasonal freshwater caps.
- These caps were hypothesized to significantly impact global ocean circulation and climate.
- The Lomonosov Ridge's location during the Eocene, between the Eurasian and Amerasian Basins, raises questions about its representativeness of the entire Arctic Ocean.
Purpose of the Study:
- To test the hypothesis of extensive Eocene Arctic Ocean freshwater caps.
- To investigate the environmental conditions of the broader Arctic Ocean during the Eocene.
- To re-evaluate the impact of Azolla events on Eocene global climate and ocean circulation.
Main Methods:
- Analysis of sediment records from the western Amerasian Basin, a region distinct from the Lomonosov Ridge.
- Examination of microfauna and allochthonous organic matter associated with Azolla remains in the Amerasian Basin sediments.
Main Results:
- Azolla events in the western Amerasian Basin were found to coincide with marine microfauna and terrestrial organic matter.
- Evidence indicates Azolla occurrences were linked to an intensified hydrologic cycle, transporting terrestrial materials into the Arctic Ocean.
- Findings suggest freshwater caps, if present, were likely restricted to the smaller Eurasian Basin.
Conclusions:
- The hypothesis of widespread Eocene Arctic freshwater caps is challenged.
- Azolla events are reinterpreted as indicators of increased riverine input driven by a stronger hydrologic cycle.
- The limited extent of potential freshwater caps suggests a restricted impact on Eocene global climate, contrary to previous models.
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