Ground ice and slope sediments archiving late Quaternary paleoenvironment and paleoclimate signals at the margins of El'gygytgyn Impact Crater, NE Siberia

youngest = 8.3 ka; accept to improve subtropical coverage

Baymag (baymag_predict.m) github.com/jesstierney/BAYMAG Parameters: omega=1.5207, salinity=35.0236, pH=8.0316, clean=0, species=ruber, pstd=10, varargin=0

Bayfoxm (byfox_predict.m) 10.1029/2019PA003576 Parameters: prior_mean=26.7011, prior_std=10, species=ruber, bayes=unspecified; For d18osw, values are specified to change through time, and are calculated using the getvardelo.m program from Jess Tierney, based on the modern value of d18osw (0.73415) for the archive location

In about 10% of the samples, pink and white ruber were combined for mg/ca analyses. Some of the d18O data are from Leventer, 1982

Flower, Benjamin P.; Hastings, David W.; Hill, Heather W.; Quinn, Terrence M.

Phasing of deglacial warming and Laurentide Ice Sheet meltwater in the Gulf of Mexico

Atlantic Ocean>North Atlantic Ocean>Gulf Of Mexico

precipitation (M2LyqvhaodqP): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Reconstructing Millennial-Scale, Regional Paleoclimates of Boreal Canada during the Holocene

<jats:p> Regional paleoclimate reconstructions for northern Canada quantify Holocene climate variability on orbital and millennial time scales and provide a context to better understand the current global warming. The reconstructions are based on available pollen diagrams from the boreal and low Arctic zones of Canada and use the modern analog technique (MAT). Four regional reconstructions document the space–time evolution of the climate during the Holocene. Highest summer and winter temperatures anomalies are found in central Canada during the early Holocene. Eastern Canada was relatively cool in the early Holocene, whereas central Canada was warmest at that time. Labrador was relatively dry in the early to mid-Holocene during which time western Canada was relatively moist. Millennial-scale temperature variations, especially the Medieval Warm Period and Little Ice Age are seen across the continent, with some suggestion of time-transgressive changes from west to east. At the millennial scale, precipitation anomalies are of opposite signs in eastern and western Canada. The results herein indicate that modern increases in temperatures in northern Canada far exceed natural millennial-scale climate variability. </jats:p>