2016
DOI: 10.1007/s10933-016-9923-1
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Lower Pahranagat Lake: modern analogue for extensive carbonate deposition in paleolakes of the Late Oligocene to Miocene Rainbow Gardens and Horse Spring Formations

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Cited by 7 publications
(14 citation statements)
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“…Hickson et al (2018) described several sedimentary facies for LPAH12-1 cores representing the last ~2000 cal yr. LPAH sediments are primarily carbonate muds and silts with some intervals showing wavy laminations and other fabrics that are interpreted as microbial in origin. Peloidal textures dominate the carbonate sediments, with some millimeter-scale irregular and wavy laminae at irregular intervals that we interpret as thin microbial mat material based on modern analogs that have been identified in the lake (see figs.…”
Section: Resultsmentioning
confidence: 99%
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“…Hickson et al (2018) described several sedimentary facies for LPAH12-1 cores representing the last ~2000 cal yr. LPAH sediments are primarily carbonate muds and silts with some intervals showing wavy laminations and other fabrics that are interpreted as microbial in origin. Peloidal textures dominate the carbonate sediments, with some millimeter-scale irregular and wavy laminae at irregular intervals that we interpret as thin microbial mat material based on modern analogs that have been identified in the lake (see figs.…”
Section: Resultsmentioning
confidence: 99%
“…We subsampled LPAH12-1B at 5 cm intervals and LPAH16-1A at 10 cm intervals for O and C stable isotopic analysis of fine-fraction (<63 µm) authigenic carbonate. Sample preparation and analysis are described in Hickson et al (2018). Analysis was primarily completed in the Stable Isotope Laboratory at the University of Minnesota where replicate analysis of 37% of 128 samples showed average standard deviations of 0.029‰ for δ 13 C and 0.147‰ for δ 18 O.…”
Section: Methodsmentioning
confidence: 99%
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“…Paces and Wurster (2014) found that modern surface waters in the PNWR are comprised of a 65:25:10 mixture of three primary spring sources, with 90% ultimately coming from a deep regional aquifer in Paleozoic carbonates, and the remaining 10% from a local aquifer in shallow Tertiary volcanics. Between 2012-2016 several sediment cores were collected from Lower Pahranagat Lake (LPAH) at the southern end of the PNWR (Hickson et al, 2018). The composite core record from LPAH spans ~5800 14 C cal yr BP (Theissen et al, in review).…”
Section: Introductionmentioning
confidence: 99%