Late Wisconsin and Holocene subalpine forests of the Markagunt Plateau of Utah, southwestern Colorado Plateau, USA

Citation
Rs. Anderson et al., Late Wisconsin and Holocene subalpine forests of the Markagunt Plateau of Utah, southwestern Colorado Plateau, USA, ARCT ANTARC, 31(4), 1999, pp. 366-378
Citations number
58
Categorie Soggetti
Multidisciplinary
Journal title
ARCTIC ANTARCTIC AND ALPINE RESEARCH
ISSN journal
15230430 → ACNP
Volume
31
Issue
4
Year of publication
1999
Pages
366 - 378
Database
ISI
SICI code
1523-0430(199911)31:4<366:LWAHSF>2.0.ZU;2-Z
Abstract
The vegetation and climatic history of subalpine forests on the Colorado Pl ateau is documented from Lowder Creek Bog and Alpine Pond on the Markagunt Plateau. Pollen and macrofossil data demonstrate substantial changes at sit es above 3150 m elevation during the last ca. 13,000 yr. During and after L ate Wisconsin deglaciation, subalpine tree species (Picea engelmannii and A bies lasiocarpa) were rare or absent near the Lowder Creek Bog site, but no narboreal species predominated. P. engelmannii-A. lasiocarpa forest became well-established there between 11,000 and 9800 yr BP and subalpine trees do minated this elevation throughout the Holocene. By ca. 8500 yr BP, however, Picea declined somewhat, with minimal pollen and macrofossil deposition oc curring between ca. 8500 and 6400 yr BP. Picea trees may have thinned durin g this time or Picea may have expanded to higher elevations during this par t of the Holocene, while Pinus ponderosa expanded at lower elevations. Thes e changes were probably driven by warmer conditions with variable precipita tion. Alternative explanations include hydroseral changes within the bog, o r insect infestation on Picea. After ca. 6400 yr BP, more consistent Picea pollen influx suggests renewed importance around the bog, which has been ma intained until the present. Abies lasiocarpa became more important after ca . 2700 yr ago. The pollen sequence supports an interpretation of high effective precipitat ion during the early Holocene, followed by warmer temperatures and somewhat variable precipitation after ca. 8500 yr BP. This sequence is most similar to other sites on and near the western, southern, and northeastern Colorad o Plateau, where the maximum influence of monsoon activity may have decline d by the end of the early Holocene. Declines in summer insolation probably contributed to Late Holocene cooling, with increasing effective precipitati on at most sites, including Lowder Creek Bog.