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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2021
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Online Access: | https://dx.doi.org/10.6084/m9.figshare.14618358 https://geolsoc.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 |
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ftdatacite:10.6084/m9.figshare.14618358 2023-05-15T18:00:49+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 Coxall, Helen K. Jones, Tom Dunkley Jones, Amy P. Lunt, Peter MacMillan, Ian Marliyani, Gayatri I. Nicholas, Christopher J. O'Halloran, Aoife Piga, Emanuela Prihardjo Sanyoto Wartono Rahardjo Pearson, Paul N. 2021 https://dx.doi.org/10.6084/m9.figshare.14618358 https://geolsoc.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 Geological Society of London Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geology FOS Earth and related environmental sciences Text article-journal Journal contribution ScholarlyArticle 2021 ftdatacite https://doi.org/10.6084/m9.figshare.14618358 2021-11-05T12:55:41Z 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). Text Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Geology FOS Earth and related environmental sciences |
spellingShingle |
Geology FOS Earth and related environmental sciences Coxall, Helen K. Jones, Tom Dunkley Jones, Amy P. Lunt, Peter MacMillan, Ian Marliyani, Gayatri I. Nicholas, Christopher J. O'Halloran, Aoife Piga, Emanuela Prihardjo Sanyoto Wartono Rahardjo Pearson, Paul N. 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 FOS Earth and related environmental sciences |
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 |
Text |
author |
Coxall, Helen K. Jones, Tom Dunkley Jones, Amy P. Lunt, Peter MacMillan, Ian Marliyani, Gayatri I. Nicholas, Christopher J. O'Halloran, Aoife Piga, Emanuela Prihardjo Sanyoto Wartono Rahardjo Pearson, Paul N. |
author_facet |
Coxall, Helen K. Jones, Tom Dunkley Jones, Amy P. Lunt, Peter MacMillan, Ian Marliyani, Gayatri I. Nicholas, Christopher J. O'Halloran, Aoife Piga, Emanuela Prihardjo Sanyoto Wartono Rahardjo Pearson, Paul N. |
author_sort |
Coxall, Helen K. |
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 |
publisher |
Geological Society of London |
publishDate |
2021 |
url |
https://dx.doi.org/10.6084/m9.figshare.14618358 https://geolsoc.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_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.14618358 |
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1766170076559441920 |