Exact(1)
Additional file 1: Chronology statistics (i.e., interseries correlation coefficient and mean sensitivity) for each seed source at each test site location.
Similar(58)
Here we present an extremely high precision 230Th chronology for archaeologically constrained coral samples from a range of occupancy sites.
A tree-ring δ18O chronology for the period 1828 2000 was developed from four Pinus merkusii trees, to find a reliable proxy for reconstructing precipitation in northwest Thailand.
Fig. 3 Chronology of the Lan Na cities. Urban morphology studies usually study on how city develop and transform to represent its embedded history.
The tree-ring δ18O chronology shows significant negative correlations with regional July October precipitation during the period 1901 2000 (r = −0.62) and with July October river flow (r = −0.54), and is in good agreement with a shorter tree-ring δ18O chronology from living Pinus kesiya in northwest Thailand.
To help understand the context and the pastoral changes, we provide a chronology of events as a general and historical framework (Figure 2). Figure 2 Chronology of events in the Changthang region from the 1950s onwards and their consequences.
Usage of this function highlights on the GICC05 chronology, for the first time for the entire last glaciation, the proposed global climate relationships during the series of large and rapid millennial stadial-interstadial events.
The 14C chronology is preferred to describe the history of the deposits since the OSL chronology, which consistently overestimates the associated radiocarbon dates, may be inaccurate due to complexities in calculating dose rates, and may in addition represent the timing of sediment deposition through the cave opening rather than sediment transport to the deposit site.
Fig. 2 Chronology of Core MD02-2503: the magnetic susceptibility of core MD02-2503 (red) (Beaufort et al. 2002) is compared to that of ODP 989 (purple) (Kennett and Ingram 1995) and 7 tie points (blue) are chosen to match the two records.
Regardless of whether one accepts a short (47.5kya) or long (55kya) chronology for Aboriginal occupation of Australia, it would now appear that the second largest marsupial to ever exist was still present for a considerable time after the first arrival of Aboriginal people.
In addition, temporal offsets between reliable 210Pb and 137Cs chronologies in the intertidal zone can be attributed to erosion of the upper part of the sedimentary record.
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