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Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology
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Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology
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Journal Article
Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology
2018
Overview
The potential link between erosion rates at the Earth’s surface and changes in global climate has intrigued geoscientists for decades
1
,
2
because such a coupling has implications for the influence of silicate weathering
3
,
4
and organic-carbon burial
5
on climate and for the role of Quaternary glaciations in landscape evolution
1
,
6
. A global increase in late-Cenozoic erosion rates in response to a cooling, more variable climate has been proposed on the basis of worldwide sedimentation rates
7
. Other studies have indicated, however, that global erosion rates may have remained steady, suggesting that the reported increases in sediment-accumulation rates are due to preservation biases, depositional hiatuses and varying measurement intervals
8
–
10
. More recently, a global compilation of thermochronology data has been used to infer a nearly twofold increase in the erosion rate in mountainous landscapes over late-Cenozoic times
6
. It has been contended that this result is free of the biases that affect sedimentary records
11
, although others have argued that it contains biases related to how thermochronological data are averaged
12
and to erosion hiatuses in glaciated landscapes
13
. Here we investigate the 30 locations with reported accelerated erosion during the late Cenozoic
6
. Our analysis shows that in 23 of these locations, the reported increases are a result of a spatial correlation bias—that is, combining data with disparate exhumation histories, thereby converting spatial erosion-rate variations into temporal increases. In four locations, the increases can be explained by changes in tectonic boundary conditions. In three cases, climatically induced accelerations are recorded, driven by localized glacial valley incision. Our findings suggest that thermochronology data currently have insufficient resolution to assess whether late-Cenozoic climate change affected erosion rates on a global scale. We suggest that a synthesis of local findings that include location-specific information may help to further investigate drivers of global erosion rates.
Reported acceleration of erosion in mountainous landscapes during the late Cenozoic is the result of combining thermochronology data with disparate exhumation histories, thereby converting spatial variations in erosion rates into temporal increases.
