Tsoyowata ash; uncalibrated 14C date indicated

uncertainty (RE8rIgewJAI): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
uncertainty (RnRTXNHq9h2): paleoData_proxyGeneral: '' has been replaced by 'chironomid'
reliable (Rtcy2uT4ykc): paleoData_proxyGeneral: '' has been replaced by 'chironomid'

A late Quaternary chironomid-inferred temperature record from the Sierra Nevada, California, with connections to northeast Pacific sea surface temperatures

<jats:title>Abstract</jats:title><jats:p>Chironomid remains from a mid-elevation lake in the Sierra Nevada, California, were used to estimate quantitative summer surface water temperatures during the past ∼15,000 yr. Reconstructed temperatures increased by ∼3°C between lake initiation and the onset of the Holocene at ∼10,600 cal yr BP (calibrated years before present). Temperatures peaked at 6500 cal yr BP, displayed high variability from 6500 to 3500 cal yr BP, and stabilized after 3500 cal yr BP. This record generally tracks reconstructed Santa Barbara Basin sea surface temperatures (SSTs) through much of the Holocene, highlighting the correspondence between SST variability and California land temperatures during this interval.</jats:p>

precipitation (M2Lydw4f4fbP): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Closed lake in bedrock basin. Physiography: rough relief in Algonquin Highlands. Surrounding vegetation: Pinus/Picea/Tsuga/Abies/Acer/Quercus.

Minor error in chronology )affecting samples 519.4 and 533 cm) corrected by OH on 2.5.2019. Note that depths are cm without intervening turbidites - absolute depth estimates are therefore larger

Norway-Swiss calibration dataset (Heiri et al. 2011). Some potentially biased samples due to human impact and dating (extrapolation below lowest dated horizon).

July air temperature, 2015 recalibrated record, some potentially biased samples due to human impact and dating

WA-PLS, Swiss-Norwegian calibration dataset as described in Heiri et al. 2011

May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
Extrapolated below oldest chronological marker
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity
May be influenced by local human activity