Tufa domes and towers are common around the margins of Winnemucca Dry Lake, Nevada,
It is increasingly important to document past records of hydrologic change in areas that are drought‐prone to better predict the region's future vulnerability to recharge and water supply. Holocene spring‐associated carbonate deposits serve as terrestrial records of water balance that can complement other local, high‐resolution proxies that are moisture‐sensitive. Here we examine two carbonate deposits (one inactive perched tufa site and one active fluvial tufa site) that form from ambient‐temperature freshwater springs, as proxies of their depositional conditions. Radiocarbon (14C) analyses of charcoal fragments from the inactive perched tufa record depositional ages of 6.2 ± 0.06 (2σ) cal ka
- Award ID(s):
- 1852564
- NSF-PAR ID:
- 10468333
- Publisher / Repository:
- Wiley
- Date Published:
- Journal Name:
- Journal of Quaternary Science
- Volume:
- 37
- Issue:
- 8
- ISSN:
- 0267-8179
- Page Range / eLocation ID:
- 1359 to 1370
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.1002/jqs.3450
