|2007 GSA Denver Annual Meeting (28–31 October 2007)|
|Paper No. 153-9|
|Presentation Time: 3:45 PM-4:00 PM|
NEW INSIGHTS FROM A CYCADOPHYTE-DOMINATED PALEOFLORA IN THE EARLY JURASSIC TALKEETNA VOLCANIC FORMATION, TALKEETNA MOUNTAINS, ALASKA
SUNDERLIN, David, Geology & Environmental Geosciences, Lafayette College, Van Wickle Hall, Easton, PA 18042, firstname.lastname@example.org and REES, P. McAllister, Geosciences, Univ of Arizona, 1040 E. 4th St, Tucson, AZ 85721|
Early Jurassic plant remains are preserved in volcaniclastic siltstones, sandstones, and moderately-developed paleosols of the Talkeetna Volcanic Formation (Peninsular Terrane) in south-central Alaska. New collections from East Boulder Creek and Hicks Creek in the southern Talkeetna Mountains north of the Matanuska Valley yield cycadophyte, pteridosperm, and conifer foliage, as well as reproductive organs and wood, from the upper third of the ~5-7 km thick formation. Their presence in beds that lack marine faunal elements indicates occasional subaerial exposure and sedimentation in what is a mostly marine oceanic arc sequence. Foliage including Cladophlebis, Otozamites, Sagenopteris, and Pagiophyllum is preserved as compressions and impressions in fluvial facies. Coalified and charcoalified wood occurs within and on top of paleosol horizons as fallen trunks up to ~78 cm in diameter but remains unidentifiable. Interbedded with paleobotanically fossiliferous beds are airfall tephra deposits with volcanic bombs and bivalve-containing beds of possible freshwater deposition. This revised list of floral elements from the Talkeetna Volcanic Formation is placed into phytogeographic context with northern continental floras and plate configurations in the Early Jurassic to test recently published models of Alaskan terrane accretion.
2007 GSA Denver Annual Meeting (28–31 October 2007)
General Information for this Meeting
|Session No. 153|
Paleontology VI: Stratigraphic and Systematic Paleontology
Colorado Convention Center: 507
1:30 PM-5:30 PM, Tuesday, 30 October 2007
Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 418
© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.