youngest calibrated age (yrs before 1950 AD)

oldest calibrated age (yrs before 1950 AD)

Metcalfe et al. 2010: age model based on 5th order polynomial fit to dates below 1.511 cm and a quadradic curve above 1.511 cm
Jones et al. 2015: Age model based on 2nd order polynomial from 0-262.21 cm then a 5th order polynomial below 262.21 cm

CAL (LPD01441887): interpretation1_scope: '' has been replaced by 'climate'
CAL (LPDe9872299): interpretation1_scope: '' has been replaced by 'climate'

Ti (LPD91196716): paleoData_notes: 'Ti_norm' has been replaced by ''
Ti (LPD91196716): paleoData_proxyDetail: 'uchannel XRF' has been replaced by 'Ti_norm'

Late Holocene climate reorganisation and the North American Monsoon

Climate variability over the last two millennia in the North American Monsoon region, recorded in laminated lake sediments from Laguna de Juanacatlán, Mexico

Note: this is a different site than the lake level record from the Lake of the Woods, Wyoming. Largest age control gap is 3390 uncal yrs, accepted with relaxing criteria: important record from the region; untenable minimum age

temperature (R05eeEJNPBo): paleoData_notes: '51 lakes from British Columbia (Palmer et al. 2002)' has been replaced by ''
temperature (R05eeEJNPBo): paleoData_proxyDetail: 'assemblage' has been replaced by '51 lakes from British Columbia (Palmer et al. 2002)'

Palmer, Samantha; Walker, Ian; Heinrichs, Markus; Hebda, Richard; Scudder, Geoffrey

Postglacial midge community change and Holocene palaeotemperature reconstructions near treeline, southern British Columbia (Canada)

lakeLevel (GH20782a02): paleoData_notes: 'Elevation below modern' has been replaced by ''
lakeLevel (GH20782a02): paleoData_proxyDetail: 'core transect' has been replaced by 'Elevation below modern'

<jats:title>Abstract</jats:title>
            <jats:p>Sediment-based reconstructions of late-Quaternary lake levels provide direct evidence of hydrologic responses to climate change, but many studies only provide approximate lake-elevation curves. Here, we demonstrate a new method for producing quantitative time series of lake elevation based on the facies and elevations of multiple cores collected from a lake's margin. The approach determines the facies represented in each core using diagnostic data, such as sand content, and then compares the results across cores to determine the elevation of the littoral zone over time. By applying the approach computationally, decisions are made systematically and iteratively using different facies classification schemes to evaluate the associated uncertainty. After evaluating our assumptions using ground-penetrating radar (GPR), we quantify past lake-elevation changes, precipitation minus evapotranspiration (Δ<jats:sub>P−ET</jats:sub>), and uncertainty in both at Lake of the Woods and Little Windy Hill Pond, Wyoming. The well-correlated (r = 0.802 ± 0.002) reconstructions indicate that water levels at both lakes fell at &amp;gt;11,300, 8000–5500, and 4700–1600 cal yr BP when Δ<jats:sub>P − ET</jats:sub> decreased to −50 to −250 mm/yr. Differences between the reconstructions are typically small (10 ± 24 mm/yr since 7000 cal yr BP), and the similarity indicates that our reconstruction method can produce statistically comparable paleohydrologic datasets across networks of sites.</jats:p>