Award Abstract # 0745877
Collaborative Research: Testing hypotheses of latest Pleistocene paleo-environmental collapse, Northern Channel Islands, California

NSF Org: EAR
Division Of Earth Sciences
Recipient: NORTHERN ARIZONA UNIVERSITY
Initial Amendment Date: April 22, 2008
Latest Amendment Date: April 22, 2008
Award Number: 0745877
Award Instrument: Standard Grant
Program Manager: Lisa Boush
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: May 1, 2008
End Date: April 30, 2012 (Estimated)
Total Intended Award Amount: $52,509.00
Total Awarded Amount to Date: $52,509.00
Funds Obligated to Date: FY 2008 = $52,509.00
History of Investigator:
  • R. Scott Anderson (Principal Investigator)
    Scott.Anderson@nau.edu
Recipient Sponsored Research Office: Northern Arizona University
601 S KNOLES DR RM 220
FLAGSTAFF
AZ  US  86011
(928)523-0886
Sponsor Congressional District: 02
Primary Place of Performance: Northern Arizona University
601 S KNOLES DR RM 220
FLAGSTAFF
AZ  US  86011
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): MXHAS3AKPRN1
Parent UEI:
NSF Program(s): GLOBAL CHANGE,
Sedimentary Geo & Paleobiology
Primary Program Source: 01000809DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1304, OTHR, 0000, EGCH
Program Element Code(s): 157700, 745900
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Testing a Hypothesis of Latest Pleistocene Paleo-environmental Collapse, Northern Channel Islands, California


This research will describe the nature and timing of dramatic paleo-environmental changes that occurred on the Northern Channel Islands (NCI) of California during the latest Pleistocene. In particular, we will test the primary hypothesis that deforestation of the islands, fluvial aggradations, landsliding, and widespread burning were synchronous events caused by a sharp change in fire regime - per haps associated with the arrival of the first humans and the extinction of mammoths. Other secondary hypotheses will be tested, including changes caused by gradual climate change, gradual climate-driven increases in fire frequency, ecosystem reduction due to sea-level rise, or an impact event at ~13ka.

Recent research on the NCI has seen a growing convergence in the ages of key events around 13, 00 cal yBP, including (1) a paleobotanical shift from conifer cover to non-arboreal vegetation, (2) onset of lowland aggradations, (3) Pleistocene landsliding: (4) deposition of charcoal and disseminated carbon; (5) arrival of the first humans, and (6) extinction of mammoths on the NCI. Another research group has suggested an impact event at ~12.9 ka. This work will test these hypotheses through: detailed description of the stratigraphy of latest Pleistocene sequences, OSL and radiocarbon dating, palynology and paleobotany, local mapping of the post-OIS2 transgression, characterization of charcoal deposition, and systematic sampling of microspherules and other potential extraterrestrial indicators through the latest Pleistocene-Holocene sequence.

Fire is a documented mechanism by which small numbers of humans may have large impacts on natural systems. Regional anthropogenic environmental impacts at the vanguard of human migration into the New World might imply a timing and magnitude not previously recognized.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Anderson, R.S., Starratt, S., Brunner Jass, R. and N. Pinter. "Fire and vegetation history on Santa Rosa Island, Channel Islands, and long-term environmental change in southern California" Journal of Quaternary Science. , 2010 DOI: 10.1002/jqs.1358
Anderson, R.S., Starratt, S., Brunner Jass, R. and N. Pinter. "Fire and vegetation history on Santa Rosa Island, Channel Islands, and long-term environmental change in southern California" Journal of Quaternary Science. , v.25 (5) , 2010 , p.782 DOI: 10.1002/jqs.1358
Pinter, N., Scott, A.C., Daulton, T.L., Podoll, A., Koeberl, C., Anderson, R.S., Ishman, S.E. "The Younger Dryas impact hypothesis: a requiem" Earth-Science Reviews , v.106 , 2011 , p.247
Pinter, N., Scott, A.C., Daulton, T.L., Podoll, A., Koeberl, C., Anderson, R.S., Ishman, S.E. "The Younger Dryas impact hypothesis: a requiem" Earth-Science Reviews , v.106 , 2011 , p.247 doi:10.1016/j.earscirev.2011.02.005
Scott, A., Pinter, N., Collinson, M., Hardiman, M., Anderson, R.S., Brain, A., Smith, S., Marone, F., Stampanoni, M "Fungus, not comet or catastrophe, accounts for carbonaceous spherules in the Younger Dryas 'impact layer'" Geophysical Research Letters. , v.37 , 2010 10.1029/2010GL043345
Scott, A., Pinter, N., Collinson, M., Hardiman, M., Anderson, R.S., Brain, A., Smith, S., Marone, F., Stampanoni, M "Fungus, not comet or catastrophe, accounts for carbonaceous spherules in the Younger Dryas 'impact layer'" Geophysical Research Letters. , v.37 , 2010 , p.L14302 10.1029/2010GL043345

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