High resolution lake sediment record reveals self-organized criticality in erosion processes regulated by internal feedbacks

D. Colombaroli, D. G. Gavin, A. E. Morey, V. R. Thorndycraft

Research output: Contribution to journalArticlepeer-review

5 Scopus citations

Abstract

Reconstruction of high-frequency erosion variability beyond the instrumental record requires well-dated, high-resolution proxies from sediment archives. We used computed tomography (CT) scans of finely laminated silt layers from a lake-sediment record in southwest Oregon to quantify the magnitude of natural landscape erosion events over the last 2000 years in order to compare with palaeorecords of climate, forest fire, and seismic triggers. Sedimentation rates were modeled from an age–depth relationship fit through five 14C dates and the 1964 AD 137Cs peak in which deposition time (yr mm-1) varied inversely with the proportion of silt sediment measured by the CT profile. This model resulted in pseudo-annual estimates of silt deposition for the last 2000 years. Silt accumulation during the past 80 years was strongly correlated with river-discharge at annual and decadal scales, revealing that erosion was highly responsive to precipitation during the logging era (1930–present). Before logging the frequency–magnitude relationship displayed a power-law distribution that is characteristic of complex feedbacks and self-regulating mechanisms. The 100-year and 10-year erosion magnitude estimated in a 99-year moving window varied by 1.7 and 1.0 orders of magnitude, respectively. Decadal erosion magnitude was only moderately positively correlated with a summer temperature reconstruction over the period 900–1900 AD. Magnitude of the seven largest events was similar to the cumulative silt accumulation anomaly, suggesting these events ‘returned the system’ to the long-term mean rate. Instead, the occurrence of most erosion events was related to fire (silt layers preceded by high charcoal concentration) and earthquakes (the seven thickest layers often match paleo-earthquake dates). Our data show how internal (i.e. sediment production) and external processes (natural fires or more stochastic events such as earthquakes) co-determine erosion regimes at millennial time scales, and the extent to which such processes can be offset by recent large-scale deforestation by logging.

Original languageEnglish (US)
Pages (from-to)2181-2192
Number of pages12
JournalEarth Surface Processes and Landforms
Volume43
Issue number10
DOIs
StatePublished - Aug 2018

Bibliographical note

Funding Information:
The study was supported by the Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, fellowship PBBEA 117553 (to D.C.) with additional support to D.G.G. from the University of Oregon and to A.E.M. from Oregon State University.

Publisher Copyright:
Copyright © 2018 John Wiley & Sons, Ltd.

Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.

Keywords

  • computed tomography
  • fire
  • hill-slope erosion
  • logging
  • self-regulating systems

Continental Scientific Drilling Facility tags

  • OSU

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