|2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM|
|Paper No. 337-5|
|Presentation Time: 9:10 AM-9:25 AM|
Permian-Pennsylvanian Climate from Paleosols in North-Central New Mexico, USA
MILLESON, Mary E., Department of Earth Sciences, Southern Methodist University, PO Box 750395, Dallas, TX 75275, firstname.lastname@example.org and TABOR, Neil J., Department of Geological Sciences, Southern Methodist University, P.O. Box 750395, Dallas, TX 75275-0395|
This study presents lithostratigraphic, mineralogic, and stable isotope proxies of equatorial paleoclimate from Upper Pennsylvanian (Missourian-Virgilian) through Lower Permian (Wolfcampian) strata of the Taos Trough, north-central New Mexico, USA. The Upper Paleozoic sequence includes mixed marine carbonate and terrestrial clastic rocks in Pennsylvanian strata (Madera Fm) which transition to terrestrial-dominated siliciclastic rocks in the Lower Permian (Sangre de Cristo Fm). Paleosol morphologies include eutric Argillisols in Missourian rocks, Calcisols in Virgilian and Wolfcampian rocks, and gypsic subgroups in upper Wolfcampian strata. X-ray diffraction analysis of pedogenic clay minerals shows a shift from kaolinite, smectite, vermiculite, and illite assemblages representative of seasonal, subhumid environments in the lower part of the stratigraphy to poorly-ordered 2:1 phyllosilicate and illite assemblages, representative of increased aridity and decreased seasonality, in the uppermost part of the stratigraphy. The stratigraphic distribution of these morphologies is suggestive of stepped change from a subhumid seasonal climate in Missourian time to a nonseasonal arid climate in end-Wolfcampian time.
There appears to be no significant stratigraphic trend among organic matter d13C values, which range from ~-22.5 to -24‰. However, paleosol calcite d13C values are ~-5‰ in Virgilian strata, ~-8‰ in lower Wolfcampian strata, and ~-5‰ in topmost Wolfcampian strata. These data suggest relatively high atmospheric PCO2 (or low biological productivity) during deposition of Pennsylvanian and upper Wolfcampian strata, and relatively low atmospheric PCO2 (or high biological productivity) during deposition of lower Wolfcampian strata. The d18O value of pedogenic calcite ranges from ~-4 to -6.5‰ throughout the Missourian, Virgilian and Wolfcampian strata. However, calcite d18O values of the top-most Wolfcampian strata range from +1 to +3‰. This stratigraphically abrupt, +5-7‰, shift in calcite d18O values is consistent with predicted changes in tropical rainfall d18O values during deglaciation of the ice-sheet in Gondwanaland.
2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
General Information for this Meeting
|Session No. 337|
Permian and Triassic Terrestrial Biotic Responses to Global Perturbations
George R. Brown Convention Center: 330A
8:00 AM-12:00 PM, Thursday, 9 October 2008
Geological Society of America Abstracts with Programs, Vol. 40, No. 6, p. 535
© Copyright 2008 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.