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A highly productive Subarctic Atlantic during the Last Interglacial and the role of diatoms

Romero, O.E.; Swann, G.E.A.; Hodell, D.A.; Helmke, P.; Rey, D.; Rubio, B.

Authors

O.E. Romero

D.A. Hodell

P. Helmke

D. Rey

B. Rubio



Abstract

The Last Interglacial (LIG), corresponding to Marine Isotope Stage (MIS) 5e, provides a reference of interglacial climate variability in the absence of anthropogenic forcing. Using an expanded section of the LIG gained at Integrated Ocean Drilling Program Site U1304 in the Subarctic Atlantic, we demonstrate that the early MIS 5e was marked by oceanographic conditions conducive for high diatom production and accumulation. The appearance of diatom-dominated laminated oozes ∼3 k.y. after the beginning of MIS 5e at ca. 125 ka coincides with a shift to higher δ30Sidiat values together with the dominance of Thalassiothrix longissima, indicative of increased nutrient availability and silicic acid utilization in surface waters. Though the Subarctic Front provided the physical conditions for high diatom production and deposition, these processes alone are insufficient to explain the high rates of siliceous productivity and the formation of diatomaceous sediments. Instead, the additional presence of an increased nutrient pool provided by Subantarctic Mode Water played the decisive role in initiating and sustaining diatom production. The high diatom productivity and the occurrence of diatomaceous sediments in the late Quaternary challenge the current hypothesis of a silica-depleted North Atlantic during the LIG.

Citation

Romero, O., Swann, G., Hodell, D., Helmke, P., Rey, D., & Rubio, B. (2011). A highly productive Subarctic Atlantic during the Last Interglacial and the role of diatoms. Geology, 39(11), 1015–1018. https://doi.org/10.1130/G32454.1

Journal Article Type Article
Acceptance Date May 31, 2011
Publication Date Nov 1, 2011
Deposit Date Feb 13, 2025
Journal Geology
Print ISSN 0091-7613
Electronic ISSN 1943-2682
Publisher Geological Society of America
Peer Reviewed Peer Reviewed
Volume 39
Issue 11
Pages 1015–1018
DOI https://doi.org/10.1130/G32454.1
Public URL https://nottingham-repository.worktribe.com/output/23525610
Publisher URL https://pubs.geoscienceworld.org/gsa/geology/article/39/11/1015/130405/A-highly-productive-Subarctic-Atlantic-during-the