Orbitally forced Azolla blooms and Middle Eocene Arctic hydrology: Clues from palynology

Autor: Barke, J., Abels, H.A., Sangiorgi, F., Greenwood, D.R., Sweet, A.R., Donders, T., Reichart, G.-J., Lotter, A.F., Brinkhuis, H., Astronomical control on classic fluvial successions in the Bighorn basin (Wyoming, USA): Implications for duration of transient global warming events and rates of mammal turnover during the early Paleogene, Biomarine Sciences, Organic geochemistry & molecular biogeology, Palaeoecology, Sub Palaeoecology begr. 01-01-12, Stratigraphy and paleontology, Sub Biomarine Sciences begr. 01-01-12, Dep Biologie, Organic geochemistry, Coastal dynamics, Fluvial systems and Global change
Přispěvatelé: Astronomical control on classic fluvial successions in the Bighorn basin (Wyoming, USA): Implications for duration of transient global warming events and rates of mammal turnover during the early Paleogene, Biomarine Sciences, Organic geochemistry & molecular biogeology, Palaeoecology, Sub Palaeoecology begr. 01-01-12, Stratigraphy and paleontology, Sub Biomarine Sciences begr. 01-01-12, Dep Biologie, Organic geochemistry, Coastal dynamics, Fluvial systems and Global change, Barke, Judith, Abels, Hemmo A, Sangiorgi, Francesca, Greenwood, David R, Sweet, Arthur R, Donders, Timme, Reichart, Gert-Jan, Lotter, André F, Brinkhuis, Henk
Jazyk: angličtina
Rok vydání: 2011
Předmět:
Zdroj: EPIC3Geology, 39(5), pp. 427-430
Geology, 5, 39, 427-430
Geology, 39(5), 427. Geological Society of America
ISSN: 0091-7613
Popis: The high abundances and cyclic distribution of remains of the freshwater fern Azolla in early-Middle Eocene sediments from the Arctic Ocean have previously been related to episodic surface-water freshening, which was speculated to be orbitally modulated. Our integrated palynological and cyclostratigraphical analysis of the recovered Azolla interval in Integrated Ocean Drilling Program (IODP) core 302-M0004A-11X resulted in the recognition of two clear periodicities: a dominant ~1.2 m cyclicity, which we relate to changes in obliquity (~40 k.y.), and a weaker ~0.7 m cyclicity, which we link to precession (~21 k.y.). Cycles in the abundances of Azolla, cysts of freshwater-tolerant dinoflagellates, and swamp-vegetation pollen show covariability in the obliquity domain. This strong correlation suggests periods of enhanced rainfall and runoff during Azolla blooms, presumably linked to increased local summer temperatures during obliquity maxima. Larix and bisaccate conifer pollen covary at the precession frequency, with peak occurrences corresponding to precession minima, possibly as a result of enhanced continental runoff from a more remote source area and a stronger seasonal contrast. Following the sudden demise of Azolla ca. 48.1 Ma, runoff (cycles) continued to influence the central Arctic at decreased intensity. This and a concomitant decline in swamp-vegetation pollen suggest edaphically drier conditions on land and decreased runoff into the Arctic Ocean, causing salinity changes, which might have been fatal for Azolla. Moreover, a sea-level rise, inferred from overall decreasing total terrestrial palynomorph concentrations, possibly facilitated oceanic connections. © 2011 Geological Society of America.
Databáze: OpenAIRE