Latest Miocene to earliest Pliocene sedimentation and climate record derived from paleosinkhole fill deposits, Gray Fossil Site, northeastern Tennessee, U.S.A.
- Permanent Link:
- Latest Miocene to earliest Pliocene sedimentation and climate record derived from paleosinkhole fill deposits, Gray Fossil Site, northeastern Tennessee, U.S.A.
- Series Title:
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Shunk, Aaron J.
Driese, Steven G.
Clark, G. Michael
- Publication Date:
- Subjects / Keywords:
- Paleosinkhole ( local )
Paleoclimate ( local )
Pliocene ( local )
Tennessee ( local )
Gray Fossil Site ( local )
- serial ( sobekcm )
- Lacustrine sediments deposited within a paleosinkhole at the Gray Fossil Site (GFS) in northeastern Tennessee, USA, provide a latest Miocene and earliest Pliocene (4.5â€“7 Ma) record of sedimentation and paleoclimate. The basal graded facies consists of mm- to cm-thick, normally graded layers of primarily locally derived terrigenous silts and fine sands with low organic content, which record storm flow influxes into a 40 m-deep paleosinkhole lake. The graded facies is overlain by the laminated facies, which is characterized by mm thick, non-graded â€œAâ€“B coupletsâ€ of abundant macerated terrestrial organic matter and fine to coarse quartz sand (A), alternating with quartz and carbonate silt (B).
Isotopic evidence for establishment of either C4-dominated or mixed C3/C4 terrestrial ecosystems is not evident at this site; Î´13C values of bulk organic matter from the basal graded facies range from âˆ’ 24â€° to âˆ’ 26â€° PDB, and decrease upsection to âˆ’ 28â€° to âˆ’ 30â€° in the organic-rich laminated facies. Isotope values covary with changes in both total organic content (TOC: 0.25â€“1 wt.% in graded facies, 2â€“12 wt.% in laminated facies) and in carbonâ€“nitrogen ratio (C / N: 1â€“2 in graded facies, 20â€“50 in laminated facies). These upsection changes in sedimentary facies and organic geochemistry within the GFS are attributed to either: (1) a climate shift characterized by increased precipitation and concomitant increased vegetation within the paleosinkhole watershed over time, or (2) progressive shallowing and eutrophication of the paleosinkhole lake, coupled with organic diagenesis within either the watershed or the paleosinkhole sediments, in which there was isotopic discrimination associated with organic matter decomposition. Subaerial exposure of the paleosinkhole lake is recorded by paleosol development.
- Original Version:
- Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 231, no. 3-4 (2006-02-28).
- Source Institution:
- University of South Florida Library
- Holding Location:
- University of South Florida
- Rights Management:
- This object is protected by copyright, and is made available here for research and educational purposes. Permission to reuse, publish, or reproduce the object beyond the bounds of Fair Use or other exemptions to copyright law must be obtained from the copyright holder.
No images or PDF downloads are available for this resource.
Cras ut cursus ante, a fringilla nunc. Mauris lorem nunc, cursus sit amet enim ac, vehicula vestibulum mi. Mauris viverra nisl vel enim faucibus porta. Praesent sit amet ornare diam, non finibus nulla.
Cras efficitur magna et sapien varius, luctus ullamcorper dolor convallis. Orci varius natoque penatibus et magnis dis parturient montes, nascetur ridiculus mus. Fusce sit amet justo ut erat laoreet congue sed a ante.
Phasellus ornare in augue eu imperdiet. Donec malesuada sapien ante, at vehicula orci tempor molestie. Proin vitae urna elit. Pellentesque vitae nisi et diam euismod malesuada aliquet non erat.
Nunc fringilla dolor ut dictum placerat. Proin ac neque rutrum, consectetur ligula id, laoreet ligula. Nulla lorem massa, consectetur vitae consequat in, lobortis at dolor. Nunc sed leo odio.