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Local variability in early Oligocene paleosols as a result of ancient soil catenary processes, Brule Formation, Toadstool Park, Nebraska

Abstract

dc:description.abstract

Paleopedology is often employed in paleoenvironmental reconstructions because the features of paleosols are affected by changes in climate, ecology, topography, and lithology over time. These changes cause small-scale variations in the morphology and apparent development of paleosols and influence the degree to which certain soil features are preserved in the rock record. When drawing inferences about paleoenvironments based on paleosols, care must be taken to ensure that as many of the soil forming factors as possible are understood. Whereas climates can be ignored over small areas, and lithology represents the medium of soil preservation, topographic relief can vary dramatically over local scales, thereby influencing the partitioning of plant communities and contributing greatly to the development of soils. In this study, paleo-geomorphological relationships were investigated along a paleovalley sequence in the Early Oligocene Orella Member of the Brule Formation in the White River G

Degree

thesis:*
Grantor dc:publisher
Temple University. Libraries
Year dc:date.issued
2011

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Kennedy, Raymond
Advisor dc:contributor.advisor
  • Terry, Dennis O., 1965-
Committee members dc:contributor.committeemember
  • Grandstaff, David E.
  • Tumarkin-Deratzian, Allison

Subjects

dc:subject × 8

Rights

dc:rights
Statement dc:rights
  • IN COPYRIGHT- This Rights Statement can be used for an Item that is in copyright. Using this statement implies that the organization making this Item available has determined that the Item is in copyright and either is the rights-holder, has obtained permission from the rights-holder(s) to make their Work(s) available, or makes the Item available under an exception or limitation to copyright (including Fair Use) that entitles it to make the Item available.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Dc Identifier Other
864885230
OAI identifier oai:identifier
oai:scholarshare.temple.edu:20.500.12613/1596

Chain of custody

source
Harvested from
Temple University
Base URL
scholarshare.temple.edu/server/oai/request
Last updated
2026-07-27
Source record
OAI-PMH GetRecord
citation

Kennedy, Raymond. Local variability in early Oligocene paleosols as a result of ancient soil catenary processes, Brule Formation, Toadstool Park, Nebraska. Temple University. Libraries, 2011. http://hdl.handle.net/20.500.12613/1596