High-precision 14C and 40Ar/39Ar dating of the Campanian Ignimbrite (Y-5) reconciles the time-scales of climatic-cultural processes at 40 ka
Language
English
Obiettivo Specifico
1V. Storia eruttiva
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
/7 (2017)
Pages (printed)
45940
Date Issued
2017
Abstract
The Late Pleistocene Campanian Ignimbrite (CI) super-eruption (Southern Italy) is the largest known
volcanic event in the Mediterranean area. The CI tephra is widely dispersed through western Eurasia
and occurs in close stratigraphic association with significant palaeoclimatic and Palaeolithic cultural
events. Here we present new high-precision 14C (34.29 ± 0.09 14C kyr BP, 1σ) and 40Ar/39Ar (39.85 ± 0.14
ka, 95% confidence level) dating results for the age of the CI eruption, which substantially improve upon
or augment previous age determinations and permit fuller exploitation of the chronological potential
of the CI tephra marker. These results provide a robust pair of 14C and 40Ar/39Ar ages for refining both
the radiocarbon calibration curve and the Late Pleistocene time-scale at ca. 40 ka. In addition, these
new age constraints provide compelling chronological evidence for the significance of the combined
influence of the CI eruption and Heinrich Event 4 on European climate and potentially evolutionary
processes of the Early Upper Palaeolithic.
volcanic event in the Mediterranean area. The CI tephra is widely dispersed through western Eurasia
and occurs in close stratigraphic association with significant palaeoclimatic and Palaeolithic cultural
events. Here we present new high-precision 14C (34.29 ± 0.09 14C kyr BP, 1σ) and 40Ar/39Ar (39.85 ± 0.14
ka, 95% confidence level) dating results for the age of the CI eruption, which substantially improve upon
or augment previous age determinations and permit fuller exploitation of the chronological potential
of the CI tephra marker. These results provide a robust pair of 14C and 40Ar/39Ar ages for refining both
the radiocarbon calibration curve and the Late Pleistocene time-scale at ca. 40 ka. In addition, these
new age constraints provide compelling chronological evidence for the significance of the combined
influence of the CI eruption and Heinrich Event 4 on European climate and potentially evolutionary
processes of the Early Upper Palaeolithic.
Type
article
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