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IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
The IntCal09 and Marine09 radiocarbon calibration curves have been revised utilizing newly available and updated data sets from 14C measurements on tree rings, plant macrofossils, speleothems,
IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP
The IntCal04 and Marine04 radiocarbon calibration curves have been updated from 12 cal kBP (cal kBP is here defined as thousands of calibrated years before AD 1950), and extended to 50 cal kBP,
SHCal13 Southern Hemisphere Calibration, 0–50,000 Years cal BP
The Southern Hemisphere SHCal04 radiocarbon calibration curve has been updated with the addition of new data sets extending measurements to 2145 cal BP and including the ANSTO Younger Dryas Huon pine
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
ABSTRACT Radiocarbon (14C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age equivalents using a
Extraction of rhyolitic component of Vedde microtephra from minerogenic lake sediments
  • C. Turney
  • Geology, Environmental Science
  • 1 February 1998
A technique is described for the extraction of rhyolitic microtephra from inorganic Lateglacial lake sediments. This technique was successfully applied by Lowe and Turney (1996) and is an adaption of
Archaeology and age of a new hominin from Flores in eastern Indonesia
TLDR
Dating by radiocarbon, luminescence, uranium-series and electron spin resonance methods indicates that H. floresiensis existed from before 38,000 years ago (kyr) until at least 18 kyr, and originated from an early dispersal of Homo erectus that reached Flores and then survived on this island refuge until relatively recently.
Does the Agulhas Current amplify global temperatures during super‐interglacials?
Future projections of climate suggest our planet is moving into a ‘super‐interglacial’. Here we report a global synthesis of ice, marine and terrestrial data from a recent palaeoclimate equivalent,
The use of microtephra horizons to correlate Late-glacial lake sediment successions in Scotland
Evidence is presented to show that two measurable concentrations of microtephra particles can be detected in deposits of Late Devensian Late-glacial age in three sites in Scotland. One layer is
Continental-scale temperature variability during the past two millennia
Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to
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