Landslide-dammed paleolake perturbs marine sedimentation and drives genetic change in anadromous fish
Abstract
Large bedrock landslides have been shown to modulate rates and processes of river activity by forming dams, forcing upstream aggradation of water and sediment, and generating catastrophic outburst floods. Less apparent is the effect of large landslide dams on river ecosystems and marine sedimentation. Combining analyses of 1-m resolution topographic data (acquired via airborne laser mapping) and field investigation, we present evidence for a large, landslide-dammed paleolake along the Eel River, CA. The landslide mass initiated from a high-relief, resistant outcrop which failed catastrophically, blocking the Eel River with an approximately 130-m-tall dam. Support for the resulting 55-km-long, 1.3-km^3 lake includes subtle shorelines cut into bounding terrain, deltas, and lacustrine sediments radiocarbon dated to 22.5 ka. The landslide provides an explanation for the recent genetic divergence of local anadromous (ocean-run) steelhead trout (Oncorhynchus mykiss) by blocking their migration route and causing gene flow between summer run and winter run reproductive ecotypes. Further, the dam arrested the prodigious flux of sediment down the Eel River; this cessation is recorded in marine sedimentary deposits as a 10-fold reduction in deposition rates of Eel-derived sediment and constitutes a rare example of a terrestrial event transmitted through the dispersal system and recorded offshore.
Additional Information
© 2011 by the National Academy of Sciences. Edited by Thomas Dunne, University of California, Santa Barbara, CA, and approved September 15, 2011 (received for review June 27, 2011). Published online before print November 14, 2011. We thank the Stewart, Lone Pine, and Island Mountain Ranches for field access. Sean Bemis processed the Center for Accelerator Mass Spectrometry ^(14)C samples. We had fruitful discussions with Harvey Kelsey and Woodward Fisher. Comments from three anonymous reviewers greatly improved this manuscript. This research was funded by National Science Foundation (NSF) Grant EAR‐0447190 (to J.J.R.), the Fulbright Earthquake Commission Scholarship from New Zealand (B.H.M.), and a Keck Institute for Space Studies Grant and NSF Grant EAR-0922199 (to M.P.L.). LiDAR data were acquired by the National Center for Airborne Laser Mapping in September 2006. Author contributions: B.H.M. and J.J.R. designed research; B.H.M. performed research; B.H.M., J.J.R., and M.P.L. analyzed data; and B.H.M. wrote the paper. The authors declare no conflict of interest. This article is a PNAS Direct Submission. This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1110445108/-/DCSupplemental.Attached Files
Published - Mackey2011p16432P_Natl_Acad_Sci_Usa.pdf
Supplemental Material - pnas.1110445108_SI.pdf
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Additional details
- PMCID
- PMC3223463
- Eprint ID
- 28426
- Resolver ID
- CaltechAUTHORS:20111212-131555415
- EAR-0447190
- NSF
- EAR-0922199
- NSF
- Fulbright Earthquake Commission
- Keck Institute for Space Studies (KISS)
- Created
-
2011-12-13Created from EPrint's datestamp field
- Updated
-
2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Keck Institute for Space Studies, Division of Geological and Planetary Sciences