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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Online Access: | https://doi.org/10.6084/m9.figshare.14617742.v2 https://figshare.com/articles/journal_contribution/_b_Supplementary_Fig_2_b_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/14617742 |
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ftgeosoclonfig:oai:figshare.com:article/14617742 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 2021-05-19T11:48:39Z https://doi.org/10.6084/m9.figshare.14617742.v2 https://figshare.com/articles/journal_contribution/_b_Supplementary_Fig_2_b_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/14617742 unknown doi:10.6084/m9.figshare.14617742.v2 https://figshare.com/articles/journal_contribution/_b_Supplementary_Fig_2_b_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/14617742 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.14617742.v2 2021-05-19T22:55:35Z 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.14617742.v2 https://figshare.com/articles/journal_contribution/_b_Supplementary_Fig_2_b_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/14617742 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
doi:10.6084/m9.figshare.14617742.v2 https://figshare.com/articles/journal_contribution/_b_Supplementary_Fig_2_b_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/14617742 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.14617742.v2 |
_version_ |
1766169660954247168 |