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Untersuchung des Potenzials eines Bohrkerns vom Paläosee Idaho als Paläoklimaarchiv Nordamerikas im Plio- und Pleistozän

Fachliche Zuordnung Paläontologie
Förderung Förderung von 2020 bis 2022
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 438282349
 
Erstellungsjahr 2022

Zusammenfassung der Projektergebnisse

We have generated a new palynological record for the late Pliocene to early Pleistocene (c. 2.8–2.4 Ma) from drillcore material from paleo-Lake Idaho (northwestern USA). Dated via paleomagnetic reversals and augmented by quantitative pollen-based climate estimates, it provides new insight into the climate and ecosystem variability in northwestern North America during the intensification of Northern Hemisphere glaciation. Our data suggest that forest dynamics were predominantly driven by climate change, likely including glacial/interglacial variability, as a response to orbital obliquity forcing. Importantly, the new pollen data from paleo-Lake Idaho document a climatically driven forest biome change across the Plio/Pleistocene boundary, which is marked by the replacement of conifer-dominated forests by open mixed forests. This change is related to an increase in moisture availability. This is in agreement with the hypothesis that moisture transport to the high latitudes of North America increased at that time due to palaeoceanographic changes in the subarctic Pacific Ocean. In addition, the estimated timing of forest-composition change at paleo-Lake Idaho at ~ 2.6 Ma is consistent with the onset of ice-rafted debris deposition in the North Pacific and a surfacetemperature drop at the California Margin. Altogether, the close correspondence between our palynological data from paleo-Lake Idaho and marine proxy records from the NE Pacific suggests a close coupling of terrestrial ecosystem change in North America to Pacific Ocean circulation dynamics across the Plio/Pleistocene boundary.

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