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A multi-proxy study of changing environmental conditions in a Younger Dryas sequence in southwestern Manitoba, Canada, and evidence for an extraterrestrial event

Published online by Cambridge University Press:  22 October 2019

James Teller ,
Matthew Boyd ,
Malcolm LeCompte ,
James Kennett ,
Allen West ,
Alice Telka ,
Aura Diaz ,
Victor Adedeji ,
Dale Batchelor  and
Charles Mooney
...Show all authors
James Teller*
Affiliation:
Department of Geological Sciences, University Manitoba, Winnipeg, Manitoba R3T 4M4, Canada
Matthew Boyd
Affiliation:
Department of Anthropology, Lakehead University, Thunder Bay, Ontario P7B 5E1, Canada
Malcolm LeCompte
Affiliation:
Center for Remote Sensing Education and Research, Elizabeth City State University, Elizabeth City, North Carolina 27909, USA
James Kennett
Affiliation:
Department of Earth Science and Marine Science Institute, University of California, Santa Barbara, California 93106, USA
Allen West
Affiliation:
Geoscience Consulting, Prescott, Arizona 86301, USA
Alice Telka
Affiliation:
Paleotec Services, Ottawa, Ontario K1R 5K2, Canada
Aura Diaz
Affiliation:
Department of Environment and Geography, University Manitoba, Winnipeg, Manitoba R3T 4M4, Canada
Victor Adedeji
Affiliation:
Department of Natural Sciences, Elizabeth City State University, Elizabeth City, North Carolina 27909, USA
Dale Batchelor
Affiliation:
EAG Laboratories Inc., Raleigh, North Carolina 27606, USA
Charles Mooney
Affiliation:
Analytical Instrumentation Facility, North Carolina State University, Raleigh, North Carolina 27695
Roberto Garcia
Affiliation:
Analytical Instrumentation Facility, North Carolina State University, Raleigh, North Carolina 27695
*
*Corresponding author e-mail address: tellerjt@ms.umanitoba.ca (J. Teller).
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Abstract

Multi-proxy analyses of a sequence spanning the Younger Dryas (YD) in the Glacial Lake Hind basin of Manitoba provides insight into regional paleohydrology and paleovegetation of meltwater rivers and lakes spanning >4000 yr; the sequence is controlled by 25 new accelerator mass spectrometry ages. This lake, dammed by the Laurentide Ice Sheet, overflowed into Lake Agassiz. The pre-YD interval records rapid sedimentation from meltwaters that headed in proglacial lakes in the Canadian Prairies that are known to have been catastrophically released when ice or sediment barriers were breached. Pollen in this phase is dominated by pre-Quaternary forms eroded from Paleocene bedrock. At the onset of the YD at ~12.8 cal ka, the sudden appearance of concentrations of nanodiamonds, high-temperature magnetic spherules, platinum, and iridium provide evidence of an extraterrestrial (ET) event that others have identified at more than 40 sites in North America. Major changes in oceans and climate, and the catastrophic outflow of nearby Lake Agassiz at the onset of the YD, may be related. Lower water levels and a reduction of Souris River inflow to Lake Hind followed, which are reflected by more clayey and organic-rich sediments and a decrease in pre-Quaternary palynomorphs. This may have resulted from the deepening of river valleys caused by the release of meltwater triggered by the ET event. Wetlands then began to develop, leading to peat deposition from 12.3 to 11 cal ka. This was followed by a fluvial episode depositing sand and then by increased Holocene aridity that resulted in accumulation of a thick sequence of dune sands. A dry woodland environment with a mix of conifers (especially Picea and Larix) and deciduous trees (especially Populus and Quercus) covered the uplands from ~13 to 10 cal ka.

Keywords

Glacial lakeManitobaYounger DryasPaleoecologyFloodsExtraterrestrial event
Type
Research Article
Information
Quaternary Research , Volume 93 , January 2020 , pp. 60 - 87
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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Footnotes

†

deceased 14 September 2019

References

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