High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis

Abstract Paleoecological studies from Rocky Mountain (USA) high elevations encompassing the previous interglacial (MIS 5e) are rare. The ~10-m composite profile from the Ziegler Reservoir fossil site (2705 m asl) of central Colorado allows us to determine paleoenvironments from Marine Oxygen Isotope...

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Published in:Quaternary Research
Main Authors: Anderson, R. Scott, Jiménez-Moreno, Gonzalo, Ager, Thomas, Porinchu, David F.
Other Authors: Denver Museum of Nature and Science, U.S. Geological Survey
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2014
Subjects:
Online Access:http://dx.doi.org/10.1016/j.yqres.2014.03.005
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spelling crcambridgeupr:10.1016/j.yqres.2014.03.005 2024-06-09T07:50:01+00:00 High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis Anderson, R. Scott Jiménez-Moreno, Gonzalo Ager, Thomas Porinchu, David F. Denver Museum of Nature and Science U.S. Geological Survey 2014 http://dx.doi.org/10.1016/j.yqres.2014.03.005 http://api.elsevier.com/content/article/PII:S0033589414000398?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589414000398?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400002490 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms http://www.elsevier.com/tdm/userlicense/1.0/ Quaternary Research volume 82, issue 3, page 542-552 ISSN 0033-5894 1096-0287 journal-article 2014 crcambridgeupr https://doi.org/10.1016/j.yqres.2014.03.005 2024-05-15T13:03:59Z Abstract Paleoecological studies from Rocky Mountain (USA) high elevations encompassing the previous interglacial (MIS 5e) are rare. The ~10-m composite profile from the Ziegler Reservoir fossil site (2705 m asl) of central Colorado allows us to determine paleoenvironments from Marine Oxygen Isotope Stages (MIS) 6– 4 using pollen zones that are approximately equivalent to marine oxygen isotope stages. During Pollen Zone (PZ) 6 time, pollen assemblages dominated by Artemisia (sagebrush) suggest that alpine tundra or steppe occurred nearby. The transition to PZ 5e was characterized by a rapid increase in tree pollen, initially Picea (spruce) and Pinus (pine) but also Quercus (oak) and Pseudotsuga menziesii (Douglas-fir). Non-arboreal pollen (NAP) types increased during PZ 5d, while Abies (fir) and Juniperus (juniper) increased during PZ 5c. Pollen evidence suggests that temperatures during PZ 5b were as cold as during PZ 6, with the site again surrounded by alpine tundra. Picea dominated during PZ 5a before the onset of cooler conditions during PZ 4. The MIS 6–MIS 5e transition here was similar to the MIS 2–MIS 1 transition at other Rocky Mountain sites. However, the Ziegler Reservoir pollen record contains evidence suggesting unexpected climatic trends at this site, including a warmer-than-expected MIS 5d and cooler-than-expected MIS 5b. Article in Journal/Newspaper Tundra Cambridge University Press Quaternary Research 82 3 542 552
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collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Paleoecological studies from Rocky Mountain (USA) high elevations encompassing the previous interglacial (MIS 5e) are rare. The ~10-m composite profile from the Ziegler Reservoir fossil site (2705 m asl) of central Colorado allows us to determine paleoenvironments from Marine Oxygen Isotope Stages (MIS) 6– 4 using pollen zones that are approximately equivalent to marine oxygen isotope stages. During Pollen Zone (PZ) 6 time, pollen assemblages dominated by Artemisia (sagebrush) suggest that alpine tundra or steppe occurred nearby. The transition to PZ 5e was characterized by a rapid increase in tree pollen, initially Picea (spruce) and Pinus (pine) but also Quercus (oak) and Pseudotsuga menziesii (Douglas-fir). Non-arboreal pollen (NAP) types increased during PZ 5d, while Abies (fir) and Juniperus (juniper) increased during PZ 5c. Pollen evidence suggests that temperatures during PZ 5b were as cold as during PZ 6, with the site again surrounded by alpine tundra. Picea dominated during PZ 5a before the onset of cooler conditions during PZ 4. The MIS 6–MIS 5e transition here was similar to the MIS 2–MIS 1 transition at other Rocky Mountain sites. However, the Ziegler Reservoir pollen record contains evidence suggesting unexpected climatic trends at this site, including a warmer-than-expected MIS 5d and cooler-than-expected MIS 5b.
author2 Denver Museum of Nature and Science
U.S. Geological Survey
format Article in Journal/Newspaper
author Anderson, R. Scott
Jiménez-Moreno, Gonzalo
Ager, Thomas
Porinchu, David F.
spellingShingle Anderson, R. Scott
Jiménez-Moreno, Gonzalo
Ager, Thomas
Porinchu, David F.
High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
author_facet Anderson, R. Scott
Jiménez-Moreno, Gonzalo
Ager, Thomas
Porinchu, David F.
author_sort Anderson, R. Scott
title High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
title_short High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
title_full High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
title_fullStr High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
title_full_unstemmed High-elevation paleoenvironmental change during MIS 6–4 in the central Rockies of Colorado as determined from pollen analysis
title_sort high-elevation paleoenvironmental change during mis 6–4 in the central rockies of colorado as determined from pollen analysis
publisher Cambridge University Press (CUP)
publishDate 2014
url http://dx.doi.org/10.1016/j.yqres.2014.03.005
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genre Tundra
genre_facet Tundra
op_source Quaternary Research
volume 82, issue 3, page 542-552
ISSN 0033-5894 1096-0287
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