Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).

The bars indicate the 95.4% probability intervals of the calendar ages in Tables 5 and 6 . OxA-37728 and OxA-37729 (which date intrusive human bone from the overlying Cardial context), OxA-5521, OxA-5541 and OxA-8670 (which reflect incomplete decontamination and are minimum ages only), and OxA-22301...

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Main Authors: João Zilhão (215800), Diego E. Angelucci (11614267), Lee J. Arnold (11614270), Francesco d’Errico (432642), Laure Dayet (793579), Martina Demuro (648258), Marianne Deschamps (4860325), Helen Fewlass (10644860), Luís Gomes (11614273), Beth Linscott (11614276), Henrique Matias (11614279), Alistair W. G. Pike (9647800), Peter Steier (254409), Sahra Talamo (116803), Eva M. Wild (11614282)
Format: Still Image
Language:unknown
Published: 2021
Subjects:
Online Access:https://doi.org/10.1371/journal.pone.0259089.g023
id ftsmithonian:oai:figshare.com:article/16889992
record_format openpolar
spelling ftsmithonian:oai:figshare.com:article/16889992 2023-05-15T16:29:56+02:00 Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber). João Zilhão (215800) Diego E. Angelucci (11614267) Lee J. Arnold (11614270) Francesco d’Errico (432642) Laure Dayet (793579) Martina Demuro (648258) Marianne Deschamps (4860325) Helen Fewlass (10644860) Luís Gomes (11614273) Beth Linscott (11614276) Henrique Matias (11614279) Alistair W. G. Pike (9647800) Peter Steier (254409) Sahra Talamo (116803) Eva M. Wild (11614282) 2021-10-27T17:35:43Z https://doi.org/10.1371/journal.pone.0259089.g023 unknown https://figshare.com/articles/figure/Chronology_and_palaeoenvironmental_context_of_the_transition_at_Gruta_do_Caldeir_o_back_chamber_/16889992 doi:10.1371/journal.pone.0259089.g023 CC BY 4.0 CC-BY Sociology Science Policy Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified two major discontinuities two key points similar persistence pattern persist beyond 39 palaeoenvironmental inferences derived magnetic susceptibility analyses last glacial maximum key evidence comes index fossils appear holocene layers abc faunal remains relate empirical difficulties go component mixing caused caldeir &# 227 associated cultural transitions sedimentation rates varied refine using radiocarbon forming sedimentation hiatuses whose traditional subdivision underwent significant disturbance expected stratigraphic order div >< p expected radiocarbon ages underlying pleistocene succession site formation issues sample association issues overlie layer eb greenland interstadial 2 global climate revealed dating anomalies exist 220 – 23 000 years ago upper palaeolithic archaeology portugal )</ p middle palaeolithic levels upper solutrean place radiocarbon ages layer eb upper pleistocene upper palaeolithic sedimentation rate whose chronology succession ’ stratigraphic integrity portugal reveal middle palaeolithic depositional disturbance dating shows anomalies consist early upper used close updated overview stone tools steep increase stands even solutrean technocomplex shelter sites method ’ karst archives incomplete decontamination human usage human settlement funerary use fully understand early neolithic critical intervals controversies surrounding carnivore activity cantabrian region caldeirão features caldeirão brings c </ bayesian modelling archaeological content applicability ) Image Figure 2021 ftsmithonian https://doi.org/10.1371/journal.pone.0259089.g023 2021-12-19T23:15:51Z The bars indicate the 95.4% probability intervals of the calendar ages in Tables 5 and 6 . OxA-37728 and OxA-37729 (which date intrusive human bone from the overlying Cardial context), OxA-5521, OxA-5541 and OxA-8670 (which reflect incomplete decontamination and are minimum ages only), and OxA-22301 (which is from a subfossil marine shell) have been excluded. Plotting of the NGRIP climate curve used CalPal (version 2017.5) [ 83 ]. The magnetic susceptibility curve is from Fig 6A , here sectioned into segments whose length has been adjusted to account for the hiatuses and the dating. Still Image Greenland NGRIP Unknown Greenland
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
topic Sociology
Science Policy
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
two major discontinuities
two key points
similar persistence pattern
persist beyond 39
palaeoenvironmental inferences derived
magnetic susceptibility analyses
last glacial maximum
key evidence comes
index fossils appear
holocene layers abc
faunal remains relate
empirical difficulties go
component mixing caused
caldeir &# 227
associated cultural transitions
sedimentation rates varied
refine using radiocarbon
forming sedimentation hiatuses
whose traditional subdivision
underwent significant disturbance
expected stratigraphic order
div >< p
expected radiocarbon ages
underlying pleistocene succession
site formation issues
sample association issues
overlie layer eb
greenland interstadial 2
global climate revealed
dating anomalies exist
220 – 23
000 years ago
upper palaeolithic archaeology
portugal )</ p
middle palaeolithic levels
upper solutrean place
radiocarbon ages
layer eb
upper pleistocene
upper palaeolithic
sedimentation rate
whose chronology
succession ’
stratigraphic integrity
portugal reveal
middle palaeolithic
depositional disturbance
dating shows
anomalies consist
early upper
used close
updated overview
stone tools
steep increase
stands even
solutrean technocomplex
shelter sites
method ’
karst archives
incomplete decontamination
human usage
human settlement
funerary use
fully understand
early neolithic
critical intervals
controversies surrounding
carnivore activity
cantabrian region
caldeirão features
caldeirão brings
c </
bayesian modelling
archaeological content
applicability )
spellingShingle Sociology
Science Policy
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
two major discontinuities
two key points
similar persistence pattern
persist beyond 39
palaeoenvironmental inferences derived
magnetic susceptibility analyses
last glacial maximum
key evidence comes
index fossils appear
holocene layers abc
faunal remains relate
empirical difficulties go
component mixing caused
caldeir &# 227
associated cultural transitions
sedimentation rates varied
refine using radiocarbon
forming sedimentation hiatuses
whose traditional subdivision
underwent significant disturbance
expected stratigraphic order
div >< p
expected radiocarbon ages
underlying pleistocene succession
site formation issues
sample association issues
overlie layer eb
greenland interstadial 2
global climate revealed
dating anomalies exist
220 – 23
000 years ago
upper palaeolithic archaeology
portugal )</ p
middle palaeolithic levels
upper solutrean place
radiocarbon ages
layer eb
upper pleistocene
upper palaeolithic
sedimentation rate
whose chronology
succession ’
stratigraphic integrity
portugal reveal
middle palaeolithic
depositional disturbance
dating shows
anomalies consist
early upper
used close
updated overview
stone tools
steep increase
stands even
solutrean technocomplex
shelter sites
method ’
karst archives
incomplete decontamination
human usage
human settlement
funerary use
fully understand
early neolithic
critical intervals
controversies surrounding
carnivore activity
cantabrian region
caldeirão features
caldeirão brings
c </
bayesian modelling
archaeological content
applicability )
João Zilhão (215800)
Diego E. Angelucci (11614267)
Lee J. Arnold (11614270)
Francesco d’Errico (432642)
Laure Dayet (793579)
Martina Demuro (648258)
Marianne Deschamps (4860325)
Helen Fewlass (10644860)
Luís Gomes (11614273)
Beth Linscott (11614276)
Henrique Matias (11614279)
Alistair W. G. Pike (9647800)
Peter Steier (254409)
Sahra Talamo (116803)
Eva M. Wild (11614282)
Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
topic_facet Sociology
Science Policy
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
two major discontinuities
two key points
similar persistence pattern
persist beyond 39
palaeoenvironmental inferences derived
magnetic susceptibility analyses
last glacial maximum
key evidence comes
index fossils appear
holocene layers abc
faunal remains relate
empirical difficulties go
component mixing caused
caldeir &# 227
associated cultural transitions
sedimentation rates varied
refine using radiocarbon
forming sedimentation hiatuses
whose traditional subdivision
underwent significant disturbance
expected stratigraphic order
div >< p
expected radiocarbon ages
underlying pleistocene succession
site formation issues
sample association issues
overlie layer eb
greenland interstadial 2
global climate revealed
dating anomalies exist
220 – 23
000 years ago
upper palaeolithic archaeology
portugal )</ p
middle palaeolithic levels
upper solutrean place
radiocarbon ages
layer eb
upper pleistocene
upper palaeolithic
sedimentation rate
whose chronology
succession ’
stratigraphic integrity
portugal reveal
middle palaeolithic
depositional disturbance
dating shows
anomalies consist
early upper
used close
updated overview
stone tools
steep increase
stands even
solutrean technocomplex
shelter sites
method ’
karst archives
incomplete decontamination
human usage
human settlement
funerary use
fully understand
early neolithic
critical intervals
controversies surrounding
carnivore activity
cantabrian region
caldeirão features
caldeirão brings
c </
bayesian modelling
archaeological content
applicability )
description The bars indicate the 95.4% probability intervals of the calendar ages in Tables 5 and 6 . OxA-37728 and OxA-37729 (which date intrusive human bone from the overlying Cardial context), OxA-5521, OxA-5541 and OxA-8670 (which reflect incomplete decontamination and are minimum ages only), and OxA-22301 (which is from a subfossil marine shell) have been excluded. Plotting of the NGRIP climate curve used CalPal (version 2017.5) [ 83 ]. The magnetic susceptibility curve is from Fig 6A , here sectioned into segments whose length has been adjusted to account for the hiatuses and the dating.
format Still Image
author João Zilhão (215800)
Diego E. Angelucci (11614267)
Lee J. Arnold (11614270)
Francesco d’Errico (432642)
Laure Dayet (793579)
Martina Demuro (648258)
Marianne Deschamps (4860325)
Helen Fewlass (10644860)
Luís Gomes (11614273)
Beth Linscott (11614276)
Henrique Matias (11614279)
Alistair W. G. Pike (9647800)
Peter Steier (254409)
Sahra Talamo (116803)
Eva M. Wild (11614282)
author_facet João Zilhão (215800)
Diego E. Angelucci (11614267)
Lee J. Arnold (11614270)
Francesco d’Errico (432642)
Laure Dayet (793579)
Martina Demuro (648258)
Marianne Deschamps (4860325)
Helen Fewlass (10644860)
Luís Gomes (11614273)
Beth Linscott (11614276)
Henrique Matias (11614279)
Alistair W. G. Pike (9647800)
Peter Steier (254409)
Sahra Talamo (116803)
Eva M. Wild (11614282)
author_sort João Zilhão (215800)
title Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
title_short Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
title_full Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
title_fullStr Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
title_full_unstemmed Chronology and palaeoenvironmental context of the transition at Gruta do Caldeirão (back chamber).
title_sort chronology and palaeoenvironmental context of the transition at gruta do caldeirão (back chamber).
publishDate 2021
url https://doi.org/10.1371/journal.pone.0259089.g023
geographic Greenland
geographic_facet Greenland
genre Greenland
NGRIP
genre_facet Greenland
NGRIP
op_relation https://figshare.com/articles/figure/Chronology_and_palaeoenvironmental_context_of_the_transition_at_Gruta_do_Caldeir_o_back_chamber_/16889992
doi:10.1371/journal.pone.0259089.g023
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1371/journal.pone.0259089.g023
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