1. Revisiting Great Basin bristlecone pine (Pinus longaeva) in the Stansbury Mountains, Utah.
- Author
-
BURCHFIELD, DAVID R., DE GROFF, OTTO W., BEKKER, MATTHEW F., KITCHEN, STANLEY G., and PETERSEN, STEVEN L.
- Subjects
- *
PINE , *GEOGRAPHIC information systems , *PLEISTOCENE-Holocene boundary , *TREE age , *BIRD migration - Abstract
Great Basin bristlecone pine (Pinus longaeva D.K. Bailey) presence in the Stansbury Mountains of northcentral Utah has been reported prior to the year 2020, but these reports lack adequate population characterization and the delineation of distinct stands of trees. In summer 2020, we identified and documented the presence of 5 separate stands of bristlecone pine in the Stansbury Mountains. These stands are removed from the nearest bristlecone populations in other mountain ranges by a distance of approximately 120 km; as such, they represent a unique outlier population of the species. We used GPS data to create a geographic information system (GIS) database delineating the 5 stands we identified, and we sampled tree age and size in one of the stands for comparison with other bristlecone pine populations in the Great Basin. We present here 2 hypotheses to explain the occurrence of bristlecone pine in the Stansbury Mountains: first, that this population is a relict from a time when bristlecone pine was widely distributed across the Great Basin; and second, that the species arrived in the range via long-distance dispersal mechanisms at some point during or after the Pleistocene/Holocene transition (ca. 12,000 14C YBP). Neotoma (woodrat) midden data suggest that bristlecone pine was absent or at least not widespread in the northern Bonneville Basin during the late Pleistocene, but midden data are sparse for the Stansbury Mountains and surrounding ranges. Additionally, we present possible migration pathways that the species could have taken to reach the Stansbury Mountains from the southern Bonneville Basin, where it was widespread during the late Pleistocene, using the largest extent of Lake Bonneville as a limiting boundary. Hypothesized migration vectors include windborne long-distance dispersal events or transport by granivorous birds. We also postulate that a small population of bristlecone pine may be present in the Oquirrh Mountains to the east of the Stansbury Mountains based upon the existence of similar habitat characteristics there, as well as our identification of a likely misdetermined 1964 voucher specimen from the Oquirrh Mountains that appears to be of bristlecone pine. [ABSTRACT FROM AUTHOR]
- Published
- 2023
- Full Text
- View/download PDF