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Title: Late Quaternary ostracode stratigraphy of Mono Lake (California, USA): evidence for benthic ecosystem sensitivity to climate change
ABSTRACT

The response of aquatic ecosystems in the Sierra Nevada (California, USA) to late Quaternary hydroclimate changes remains mostly unknown. Mono Lake, a large endorheic lake just east of the Sierra Nevada, contains an expanded archive of laminated sediments that can be used to examine the response of benthos to environmental changes. Fossil ostracodes from a radiocarbon‐dated core were used to examine paleoecologic changes from ~16.6 to 4.3k cal abp.Seven species were identified, with the co‐occurrence ofLimnocythere ceriotuberosaandLimnocythere stapliniindicating a large SO42−‐rich lake in the Pleistocene. The Younger Dryas was complex, withFabaeformiscandona caudatareflecting a cold and deep lake ~13.0–12.2k cal abp, followed by an interval of extensive littoral habitat from ~12.2–11.6k cal abp.Ostracode diversity, valves g–1and the ratio of adult:juvenile valves declined after ~10.7k cal abpdue to regression, altered hydrochemistry and seasonal anoxia. Strong seasonality during the Early Holocene is suggested by the presence of reworked ostracodes and macrocharcoal, delivered to Mono Lake by erosion of ancient lake beds in the basin. A depauperate ostracode fauna in the Middle Holocene suggests a strong sensitivity to drought in this ecosystem, which has implications for biodiversity in the future.

 
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NSF-PAR ID:
10492354
Author(s) / Creator(s):
 ;  ;  ;  ;  ;  ;  
Publisher / Repository:
Wiley Blackwell (John Wiley & Sons)
Date Published:
Journal Name:
Journal of Quaternary Science
ISSN:
0267-8179
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
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