Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes

Supplementary Fig. 2 . An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1'). Age-depth tie points are plotted as event mid-points (see Table 3) with associated depth error ranges shown. T = top, B = base. Planktonic foraminifera biozones are shown against...

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Main Authors: Helen K. Coxall, Tom Dunkley Jones, Amy P. Jones, Peter Lunt, Ian MacMillan, Gayatri I. Marliyani, Christopher J. Nicholas, Aoife O'Halloran, Emanuela Piga, Prihardjo Sanyoto, Wartono Rahardjo, Paul N. Pearson
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2021
Subjects:
HCO
NKK
Online Access:https://doi.org/10.6084/m9.figshare.14618358.v1
https://figshare.com/articles/journal_contribution/Supplementary_Fig_2_An_alternative_biostratigraphic_age_model_for_the_NKK-1_borehole_age_model_Option-1_The_Eocene_Oligocene_Transition_in_Nanggulan_Java_lithostratigraphy_biostratigraphy_and_foraminiferal_stable_isotopes/14618358
id ftgeosoclonfig:oai:figshare.com:article/14618358
record_format openpolar
spelling ftgeosoclonfig:oai:figshare.com:article/14618358 2023-05-15T18:00:32+02:00 Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes Helen K. Coxall Tom Dunkley Jones Amy P. Jones Peter Lunt Ian MacMillan Gayatri I. Marliyani Christopher J. Nicholas Aoife O'Halloran Emanuela Piga Prihardjo Sanyoto Wartono Rahardjo Paul N. Pearson 2021-05-19T13:48:53Z https://doi.org/10.6084/m9.figshare.14618358.v1 https://figshare.com/articles/journal_contribution/Supplementary_Fig_2_An_alternative_biostratigraphic_age_model_for_the_NKK-1_borehole_age_model_Option-1_The_Eocene_Oligocene_Transition_in_Nanggulan_Java_lithostratigraphy_biostratigraphy_and_foraminiferal_stable_isotopes/14618358 unknown doi:10.6084/m9.figshare.14618358.v1 https://figshare.com/articles/journal_contribution/Supplementary_Fig_2_An_alternative_biostratigraphic_age_model_for_the_NKK-1_borehole_age_model_Option-1_The_Eocene_Oligocene_Transition_in_Nanggulan_Java_lithostratigraphy_biostratigraphy_and_foraminiferal_stable_isotopes/14618358 CC BY 4.0 CC-BY Geology nannofossil zone distribution isotopes Supplementary Fig Dashed biozone separators HCO Planktonic foraminifera biozones alternative biostratigraphic age model depth error ranges Psuedohastigerina naguewichiensis r. age model Other planktonic foraminiferal events NKK certainty bioevent positions Text Journal contribution 2021 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.14618358.v1 2021-05-19T22:55:33Z Supplementary Fig. 2 . An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1'). Age-depth tie points are plotted as event mid-points (see Table 3) with associated depth error ranges shown. T = top, B = base. Planktonic foraminifera biozones are shown against the age scale. See Fig. 6 for nannofossil zone distribution. Grey circles identify the calibrated datum events used to constrain the numerical age model. Other planktonic foraminiferal events used in to construct the biozonation are also named. Dashed biozone separators indicate low certainty bioevent positions in the core. HCO = highest common occurrence, and is an alternative interpretation of the Psuedohastigerina naguewichiensis range data, using the HCO of this species as the calibrated age-depth tie-point rather than the last rare occurrence above the sandstone/basalt (Option - 2). Other Non-Article Part of Journal/Newspaper Planktonic foraminifera Geological Society of London: Figshare
institution Open Polar
collection Geological Society of London: Figshare
op_collection_id ftgeosoclonfig
language unknown
topic Geology
nannofossil zone distribution
isotopes Supplementary Fig
Dashed biozone separators
HCO
Planktonic foraminifera biozones
alternative biostratigraphic age model
depth error ranges
Psuedohastigerina naguewichiensis r.
age model
Other planktonic foraminiferal events
NKK
certainty bioevent positions
spellingShingle Geology
nannofossil zone distribution
isotopes Supplementary Fig
Dashed biozone separators
HCO
Planktonic foraminifera biozones
alternative biostratigraphic age model
depth error ranges
Psuedohastigerina naguewichiensis r.
age model
Other planktonic foraminiferal events
NKK
certainty bioevent positions
Helen K. Coxall
Tom Dunkley Jones
Amy P. Jones
Peter Lunt
Ian MacMillan
Gayatri I. Marliyani
Christopher J. Nicholas
Aoife O'Halloran
Emanuela Piga
Prihardjo Sanyoto
Wartono Rahardjo
Paul N. Pearson
Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
topic_facet Geology
nannofossil zone distribution
isotopes Supplementary Fig
Dashed biozone separators
HCO
Planktonic foraminifera biozones
alternative biostratigraphic age model
depth error ranges
Psuedohastigerina naguewichiensis r.
age model
Other planktonic foraminiferal events
NKK
certainty bioevent positions
description Supplementary Fig. 2 . An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1'). Age-depth tie points are plotted as event mid-points (see Table 3) with associated depth error ranges shown. T = top, B = base. Planktonic foraminifera biozones are shown against the age scale. See Fig. 6 for nannofossil zone distribution. Grey circles identify the calibrated datum events used to constrain the numerical age model. Other planktonic foraminiferal events used in to construct the biozonation are also named. Dashed biozone separators indicate low certainty bioevent positions in the core. HCO = highest common occurrence, and is an alternative interpretation of the Psuedohastigerina naguewichiensis range data, using the HCO of this species as the calibrated age-depth tie-point rather than the last rare occurrence above the sandstone/basalt (Option - 2).
format Other Non-Article Part of Journal/Newspaper
author Helen K. Coxall
Tom Dunkley Jones
Amy P. Jones
Peter Lunt
Ian MacMillan
Gayatri I. Marliyani
Christopher J. Nicholas
Aoife O'Halloran
Emanuela Piga
Prihardjo Sanyoto
Wartono Rahardjo
Paul N. Pearson
author_facet Helen K. Coxall
Tom Dunkley Jones
Amy P. Jones
Peter Lunt
Ian MacMillan
Gayatri I. Marliyani
Christopher J. Nicholas
Aoife O'Halloran
Emanuela Piga
Prihardjo Sanyoto
Wartono Rahardjo
Paul N. Pearson
author_sort Helen K. Coxall
title Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
title_short Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
title_full Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
title_fullStr Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
title_full_unstemmed Supplementary Fig. 2. An alternative biostratigraphic age model for the NKK-1 borehole (age model 'Option-1').The Eocene–Oligocene Transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
title_sort supplementary fig. 2. an alternative biostratigraphic age model for the nkk-1 borehole (age model 'option-1').the eocene–oligocene transition in nanggulan, java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
publishDate 2021
url https://doi.org/10.6084/m9.figshare.14618358.v1
https://figshare.com/articles/journal_contribution/Supplementary_Fig_2_An_alternative_biostratigraphic_age_model_for_the_NKK-1_borehole_age_model_Option-1_The_Eocene_Oligocene_Transition_in_Nanggulan_Java_lithostratigraphy_biostratigraphy_and_foraminiferal_stable_isotopes/14618358
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation doi:10.6084/m9.figshare.14618358.v1
https://figshare.com/articles/journal_contribution/Supplementary_Fig_2_An_alternative_biostratigraphic_age_model_for_the_NKK-1_borehole_age_model_Option-1_The_Eocene_Oligocene_Transition_in_Nanggulan_Java_lithostratigraphy_biostratigraphy_and_foraminiferal_stable_isotopes/14618358
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.14618358.v1
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