paleolithic archaeology
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2021 ◽  
Vol 50 (1) ◽  
pp. 187-202
Author(s):  
Joanne P. Baron

The philosophy of Charles S. Peirce, and in particular his theory of signs (semiotic), has seen increasing interest within archaeological theory over the past 20 years. This article reviews Peirce's most influential ideas within archaeology, directs readers to where in Peirce's voluminous works they can find these ideas, and discusses how each of them has been applied by archaeologists to a variety of different research topics. In addition to the semiotic, these ideas include Peirce's metaphysical doctrine of synechism; his methodological pragmatism; abductive logic; and the phenomenological concepts of firstness, secondness, and thirdness. Finally, I discuss two research areas—materiality and paleolithic archaeology—in which a combination of Peirce's ideas has led to important new insights.


Radiocarbon ◽  
2020 ◽  
Vol 62 (4) ◽  
pp. 1095-1117 ◽  
Author(s):  
J van der Plicht ◽  
C Bronk Ramsey ◽  
T J Heaton ◽  
E M Scott ◽  
S Talamo

ABSTRACTThe curves recommended for calibrating radiocarbon (14C) dates into absolute dates have been updated. For calibrating atmospheric samples from the Northern Hemisphere, the new curve is called IntCal20. This is accompanied by associated curves SHCal20 for the Southern Hemisphere, and Marine20 for marine samples. In this “companion article” we discuss advances and developments that have led to improvements in the updated curves and highlight some issues of relevance for the general readership. In particular the dendrochronological based part of the curve has seen a significant increase in data, with single-year resolution for certain time ranges, extending back to 13,910 calBP. Beyond the tree rings, the new curve is based upon an updated combination of marine corals, speleothems, macrofossils, and varved sediments and now reaches back to 55,000 calBP. Alongside these data advances, we have developed a new, bespoke statistical curve construction methodology to allow better incorporation of the diverse constituent records and produce a more robust curve with uncertainties. Combined, these data and methodological advances offer the potential for significant new insight into our past. We discuss some implications for the user, such as the dating of the Santorini eruption and also some consequences of the new curve for Paleolithic archaeology.


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