ome Scores, reconstructed (BS) * PI: Tarasov, Pavel E (ptarasov@zedat.fu-berlin.de, http://www.geo.fu-berlin.de/geol/fachrichtungen/pal/mitarbeiter/tarasov/index.html) * METHOD: Calculated * COMMENT: Landscape Openness

MAP (LPD6fdee25b): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Stebich, Martina; Rehfeld, Kira; Schl _tz, Frank; Tarasov, Pavel E.; Liu, Jiaqi; Mingram, Jens

Holocene vegetation and climate dynamics of NE China based on the pollen record from Sihailongwan Maar Lake

The melt layers are considered better temperature records than ice d18O, due to the strong influence of adjacent sea ice (AJO)

WEB8d90dc28: The "raw" meltlayers were made the "primary" temp12k dataset following the practice that generally, less processed data should be highlighted. It should be noted that in many circumstances, however, that a running frequency is more appropriate. Thanks to Stephen McIntyre (@ClimateAudit on twitter) for the suggestion.

meltLayers (WEB8d90dc28): paleoData_inCompilation: '' has been replaced by 'Temp12k'
meltLayers (WEB8d90dc28): paleoData_QCCertification: '' has been replaced by 'AJO'
meltLayers (WEB8d90dc28): paleoData_QCnotes: '' has been replaced by 'The melt layers are considered better temperature records than ice d18O, due to the strong influence of adjacent sea ice (AJO)'
meltLayerFrequency (WEBe15adc6e): paleoData_inCompilation: 'Temp12k' has been replaced by ''

Rise in frequency of surface melting at Siple Dome through the Holocene: Evidence for increasing marine influence on the climate of West Antarctica

precipitation (M2Ll0uq2vy4P): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Stratigraphy and genesis of the Lake Sixteen peatland, northern Michigan

Small lake in peatland. Physiography: low relief with sand ridges. Surrounding vegetation: Pinus/Quercus/Betula/Populus.

In the LiPD file the 2nd record based on chironomids, the others are unknown.

Peter Rosen; Ulf Segerstroem; Lars Eriksson; Ingemar Renberg

Do diatom, chironomid, and pollen records consistently infer Holocene July air temperature? A comparison using sediment cores from four alpine lakes in northern Sweden