Climate change at the 4.2 ka BP termination of the Indus Valley civilization and Holocene South Asian monsoon variability

Sample thickness varies throughout core; lowermost 4 ages based on interpolation

139-lake Finnish calibration dataset (Luoto et al. 2014a, 2014b)

Higher-resolution record and updated reconstruction compared to Engels et al. 2014 paper

Shala, Shyhrete; Helmens, Karin F; Luoto, Tomi P; Salonen, J Sakari; V _liranta, Minna; Weckstr̦m, Jan

Comparison of quantitative Holocene temperature reconstructions using multiple proxies from a northern boreal lake

Uncertainties should not be considered as standard deviations. Posterior distribution of temperature probabilities are highly irregular and skewed.

composite of several sites, mainly wetlands rather than lakes; age control difficult to tabulate

IMPORTANT: Please enter C14 Radiocarbon dates as UNCALIBRATED where at all possible

uncertaintyHigh (RjfQ0hW1CDk): paleoData_proxyGeneral: '' has been replaced by 'pollen'
uncertaintyLow (RX6Nm8zR9R9): paleoData_proxyGeneral: '' has been replaced by 'pollen'
DateID (RYSw8WoYURG): paleoData_proxyGeneral: '' has been replaced by 'pollen'
ReliabIeYN1 (RzZT156KspA): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Southeast African records reveal a coherent shift from high- to low-latitude forcing mechanisms along the east African margin across last glacial   interglacial transition

previously marked as "annual", but probably not

this timeseries was composited from two sites in southern california

timeseries was composited from two sites in southern california (lat/long/elevation is for one site)

Panom (LPD387da3e90): paleoData_proxyGeneral: '' has been replaced by 'pollen'
Tanom (LPD537be86c): paleoData_proxyGeneral: '' has been replaced by 'pollen'
Tanom (LPDb59e4b87): paleoData_proxyGeneral: '' has been replaced by 'pollen'
Panom (LPDf970effe1): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Review of probabilistic pollen-climate transfer methods

author's say, "Delta 18O values are interpreted as having a first order positive relationship to temperature, but also to be influenced by precipitation in a complex manner."