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The impact of humans on continental erosion and sedimentation

Bruce H. Wilkinson and Brandon J. McElroy
The impact of humans on continental erosion and sedimentation
Geological Society of America Bulletin (January 2007) 119 (1-2): 140-156

Abstract

Rock uplift and erosional denudation of orogenic belts have long been the most important geologic processes that serve to shape continental surfaces, but the rate of geomorphic change resulting from these natural phenomena has now been outstripped by human activities associated with agriculture, construction, and mining. Although humans are now the most important geomorphic agent on the planet's surface, natural and anthropogenic processes serve to modify quite different parts of Earth's landscape. In order to better understand the impact of humans on continental erosion, we have examined both long-term and short-term data on rates of sediment transfer in response to glacio-fluvial and anthropogenic processes. Phanerozoic rates of subaerial denudation inferred from preserved volumes of sedimentary rock require a mean continental erosion rate on the order of 16 m per million years (m/m.y.), resulting in the accumulation of approximately 5 gigatons of sediment per year (Gt/yr). Erosion irregularly increased over the approximately 542 m.y. span of Phanerozoic time to a Pliocene value of 53 m/m.y. (16 Gt/yr). Current estimates of large river sediment loads are similar to this late Neogene value, and require net denudation of ice-free land surfaces at a rate of approximately 62 m/m.y. ( approximately 21 Gt/yr). Consideration of the variation in large river sediment loads and the geomorphology of respective river basin catchments suggests that natural erosion is primarily confined to drainage headwaters; approximately 83% of the global river sediment flux is derived from the highest 10% of Earth's surface. Subaerial erosion as a result of human activity, primarily through agricultural practices, has resulted in a sharp increase in net rates of continental denudation; although less well constrained than estimates based on surviving rock volumes or current river loads, available data suggest that present farmland denudation is proceeding at a rate of approximately 600 m/m.y. ( approximately 75 Gt/yr), and is largely confined to the lower elevations of Earth's land surface, primarily along passive continental margins; approximately 83% of cropland erosion occurs over the lower 65% of Earth's surface. The conspicuous disparity between natural sediment fluxes suggested by data on rock volumes and river loads ( approximately 21 Gt/yr) and anthropogenic fluxes inferred from measured and modeled cropland soil losses (75 Gt/yr) is readily resolved by data on thicknesses and ages of alluvial sediment that has been deposited immediately downslope from eroding croplands over the history of human agriculture. Accumulation of postsettlement alluvium on higher-order tributary channels and floodplains (mean rate approximately 12,600 m/m.y.) is the most important geomorphic process in terms of the erosion and deposition of sediment that is currently shaping the landscape of Earth. It far exceeds even the impact of Pleistocene continental glaciers or the current impact of alpine erosion by glacial and/or fluvial processes. Conversely, available data suggest that since 1961, global cropland area has increased by approximately 11%, while the global population has approximately doubled. The net effect of both changes is that per capita cropland area has decreased by approximately 44% over this same time interval; approximately 1% per year. This is approximately 25 times the rate of soil area loss anticipated from human denudation of cropland surfaces. In a context of per capita food production, soil loss through cropland erosion is largely insignificant when compared to the impact of population growth.


ISSN: 0016-7606
EISSN: 1943-2674
Serial Title: Geological Society of America Bulletin
Serial Volume: 119
Serial Issue: 1-2
Title: The impact of humans on continental erosion and sedimentation
Affiliation: Syracuse University, Department of Earth Sciences, Syracuse, NY, United States
Pages: 140-156
Published: 200701
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
References: 81
Accession Number: 2007-014831
Categories: Geomorphology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: sketch maps
Secondary Affiliation: University of Texas, Austin, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by the Geological Society of America, Boulder, CO, United States
Update Code: 200705
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