1. Glacial Erosion Rates Since the Last Glacial Maximum for the Former Argentino Glacier and Present‐Day Upsala Glacier, Patagonia
- Author
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Fedotova, A. and Magnani, M. B.
- Abstract
Recovering the patterns of glacial erosion over time is key to understanding feedbacks between climate and tectonic processes. Glacial erosion rates have been shown to systematically increase worldwide toward the present since the late Cenozoic, a behavior interpreted as the response of glaciers to a cooling and increasingly variable climate. However, the validity of this signal has been questioned, and suggested to be affected by the incompleteness of the sedimentary record, which can introduce a time dependent bias in the time averaged rates. In this study, we present new glacial erosion rates estimated from sediment accumulations in Lago Argentino, Patagonia, a proglacial basin with a nearly complete preserved sedimentary record. The erosion rates are estimated through the past 20,000 years and averaged over time intervals ranging from sub‐decadal to millennial, allowing us to explore erosion rate variability through time and within a glacial cycle. The data show that erosion rates have varied substantially, from 0.43 ±$\pm $0.12 to 82.38 ±$\pm $17.58 mm/yr, with no systematic increase (or decrease) through time. Rather, erosion occurs during discrete, intense events separated by times of quiescence. In addition, we find that glacial erosion rates have comparable magnitudes when averaged over similar time intervals. Our data show a power‐law increase in glacial erosion rates with decreasing averaging time interval, consistent with other observations globally. Given our observed intermittent character of glacial erosion, we attribute this increase to a time averaging bias, rather than to an escalation in magnitude of erosional pulses toward the present. Glaciers are powerful agents of erosion and sensitive to climate. Their action competes with tectonic forces in limiting the heights of mountains. Understanding how fast glaciers carve into the landscape over time helps us understand the relationship between climate and tectonics. Glacial erosion rates have been shown to increase over the past 10 million years, interpreted as an effect of a cooling climate worldwide. The same signal has been interpreted to result from how rates are estimated, particularly if rates are averaged over time intervals that contain periods of low or no erosion. In this study, we present glacial erosion rates calculated from data imaging glacial sediments preserved in a lake in Patagonia, Argentina. To understand the effect of the time interval length, we calculate glacial erosion rates for the past 20,000 years over different time intervals. We find that rates show no straightforward increase toward the present. Rather, erosion occurs during discrete events separated by times of low erosion. Rates positively correlate with the length of the averaging time interval. We attribute this behavior to a bias resulting from the length of time over which erosion rates are averaged, rather than a genuine signal in erosion rate trends. Glacial erosion rates estimated over decadal to millennial time scales do not systematically increase toward the presentArgentino and Upsala Glacier erosion rates are timescale dependent, but age independentEstimated glacial erosion rates are affected by a time bias due to the intermittent character of glacial erosion Glacial erosion rates estimated over decadal to millennial time scales do not systematically increase toward the present Argentino and Upsala Glacier erosion rates are timescale dependent, but age independent Estimated glacial erosion rates are affected by a time bias due to the intermittent character of glacial erosion
- Published
- 2024
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