The detailed palaeoecology of a mid‐Wisconsinan interstadial (ca. 32 000 14 C a BP) vegetation surface from interior Alaska

Abstract We present a multi‐proxy reconstruction from a well‐preserved vegetation surface (ca. 32 000 14 C a BP) from the Fox Permafrost tunnel near Fairbanks, Alaska. A thick litter layer of plant material on the vegetation surface is consistent with the vegetation lacking evidence of disturbance....

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Wooller, Matthew J., Zazula, Grant D., Blinnikov, Misha., Gaglioti, Benjamin. V., Bigelow, Nancy. H., Sanborn, Paul., Kuzmina, Svetlana., La Farge, Catherine.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
Subjects:
Fairbanks
permafrost
Alaska
Beringia
Online Access:http://dx.doi.org/10.1002/jqs.1497
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1497
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1497
Description
Summary:Abstract We present a multi‐proxy reconstruction from a well‐preserved vegetation surface (ca. 32 000 14 C a BP) from the Fox Permafrost tunnel near Fairbanks, Alaska. A thick litter layer of plant material on the vegetation surface is consistent with the vegetation lacking evidence of disturbance. Plant macrofossils and graminoid cuticle analysis show the presence of a graminoid assemblage consistent with phytolith data. The pollen data indicate that trees were not local to the site and that Artemisia sp. was present in the region. The insect and bryophyte reconstructions are consistent with the vascular plant reconstruction, indicating the site was at least periodically wet. δ 13 C values from the graminoids present show a large range encompassing both the wet and dry range displayed by modern graminoids in Alaska. Sequential δ 13 C analyses conducted along the length of leaves attached to the vegetation surface indicate a seasonal shift towards relatively higher water use efficiency. The lower water use efficiency earlier in the growing season may have stemmed from the use of winter season meltwater by plants at the site – a scenario consistent with the site's cryostratigraphy. Our multi‐proxy reconstruction contributes to the limited palaeoecological data available for graminoid‐dominated vegetation present in Eastern Beringia and particularly the interior of Alaska during the mid‐Wisconsinan interstadial. Copyright © 2011 John Wiley & Sons, Ltd.

Similar Items