Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...

Paleobotanical site information, terpenoid, n-alkane, and other and biomarker quantification and carbon isotope data from sediment samples collected from North America Paleogene fossil leaf sites that extend from Colorado to the High Arctic. Sediment samples were collected laterally along fossil lea...

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Main Authors: Schlanser, Kristen M, Diefendorf, Aaron F, West, Christopher K, Greenwood, David R, Basinger, James F, Meyer, Herbert W, Lowe, Alexander J, Naake, Hans H
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
AGE
Fid
Online Access:https://dx.doi.org/10.1594/pangaea.919135
https://doi.pangaea.de/10.1594/PANGAEA.919135
id ftdatacite:10.1594/pangaea.919135
record_format openpolar
spelling ftdatacite:10.1594/pangaea.919135 2024-09-09T19:27:33+00:00 Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ... Schlanser, Kristen M Diefendorf, Aaron F West, Christopher K Greenwood, David R Basinger, James F Meyer, Herbert W Lowe, Alexander J Naake, Hans H 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.919135 https://doi.pangaea.de/10.1594/PANGAEA.919135 en eng PANGAEA https://dx.doi.org/10.1016/j.orggeochem.2020.104069 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 carbon isotope conifers n-alkane Paleogene terpenoid Sample ID Latitude of event Longitude of event Event label Site Location Epoch AGE Age, maximum/old Age, minimum/young Lithology/composition/facies Vegetation type Thermal maturity, hopane Pristane/Phytane ratio Carbon Preference Index Terrigenous/aquatic ratio Average chain length Carbon, organic, total Diterpenoids, plant-derived Triterpenoids, plant-derived Long-chain n-alkanes, C27-C35 Isonorpimarane, δ13C Norpimarane, δ13C 18-Norisopimarane, δ13C Tetracyclic diterpane, δ13C ent-Beyerane, δ13C 13alphaH-Fichtelite, δ13C 19-Norabieta-8,11,13-triene, δ13C 19-Norabieta-4,8,11,13-tetraene, δ13C 19-Norabieta-3,8,11,13-tetraene, δ13C 18-Norabieta-8,11,13-triene, δ13C Isopimarane, δ13C Pimarane, δ13C Abietane, δ13C ent-13-epi manoyl oxide, δ13C 2-Methyl-1-4'-methylpentyl-6-isopropylnaphthalene, δ13C Abieta-8,11,13-triene, δ13C Dehydroicetexane, δ13C 1,2,3,4-Tetrahydroretene, δ13C Simonellite, δ13C Diaromatic tricyclic totarane, δ13C Retene, δ13C Des-A-lupane, δ13C Des-A-26-norlupa-5,7,9-triene, δ13C δ13C dataset Dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.91913510.1016/j.orggeochem.2020.104069 2024-08-01T10:54:44Z Paleobotanical site information, terpenoid, n-alkane, and other and biomarker quantification and carbon isotope data from sediment samples collected from North America Paleogene fossil leaf sites that extend from Colorado to the High Arctic. Sediment samples were collected laterally along fossil leaf-bearing zones. To disentangle the vegetation source of sediment n-alkanes, we measured the carbon isotope (δ13C) values of nonsteroidal triterpenoids (angiosperm biomarkers) and tricyclic diterpenoids (conifer biomarkers) to determine angiosperm and conifer end member δ13C values. Compounds were isolated using column chromatography and identified and quantified with an Agilent 7890A gas chromatograph (GC) interfaced to an Agilent 5975C quadrupole mass selective detector (MSD) and flame ionization detector (FID). Compound-specific carbon isotope analyses were performed, where possible, on n-C27 through n-C35 alkanes, diterpenoids, and triterpenoids by gas chromatograph-combustion-isotope ratio mass spectrometry ... Dataset Arctic DataCite Arctic Fid ENVELOPE(-65.939,-65.939,-68.664,-68.664)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic carbon isotope
conifers
n-alkane
Paleogene
terpenoid
Sample ID
Latitude of event
Longitude of event
Event label
Site
Location
Epoch
AGE
Age, maximum/old
Age, minimum/young
Lithology/composition/facies
Vegetation type
Thermal maturity, hopane
Pristane/Phytane ratio
Carbon Preference Index
Terrigenous/aquatic ratio
Average chain length
Carbon, organic, total
Diterpenoids, plant-derived
Triterpenoids, plant-derived
Long-chain n-alkanes, C27-C35
Isonorpimarane, δ13C
Norpimarane, δ13C
18-Norisopimarane, δ13C
Tetracyclic diterpane, δ13C
ent-Beyerane, δ13C
13alphaH-Fichtelite, δ13C
19-Norabieta-8,11,13-triene, δ13C
19-Norabieta-4,8,11,13-tetraene, δ13C
19-Norabieta-3,8,11,13-tetraene, δ13C
18-Norabieta-8,11,13-triene, δ13C
Isopimarane, δ13C
Pimarane, δ13C
Abietane, δ13C
ent-13-epi manoyl oxide, δ13C
2-Methyl-1-4'-methylpentyl-6-isopropylnaphthalene, δ13C
Abieta-8,11,13-triene, δ13C
Dehydroicetexane, δ13C
1,2,3,4-Tetrahydroretene, δ13C
Simonellite, δ13C
Diaromatic tricyclic totarane, δ13C
Retene, δ13C
Des-A-lupane, δ13C
Des-A-26-norlupa-5,7,9-triene, δ13C
δ13C
spellingShingle carbon isotope
conifers
n-alkane
Paleogene
terpenoid
Sample ID
Latitude of event
Longitude of event
Event label
Site
Location
Epoch
AGE
Age, maximum/old
Age, minimum/young
Lithology/composition/facies
Vegetation type
Thermal maturity, hopane
Pristane/Phytane ratio
Carbon Preference Index
Terrigenous/aquatic ratio
Average chain length
Carbon, organic, total
Diterpenoids, plant-derived
Triterpenoids, plant-derived
Long-chain n-alkanes, C27-C35
Isonorpimarane, δ13C
Norpimarane, δ13C
18-Norisopimarane, δ13C
Tetracyclic diterpane, δ13C
ent-Beyerane, δ13C
13alphaH-Fichtelite, δ13C
19-Norabieta-8,11,13-triene, δ13C
19-Norabieta-4,8,11,13-tetraene, δ13C
19-Norabieta-3,8,11,13-tetraene, δ13C
18-Norabieta-8,11,13-triene, δ13C
Isopimarane, δ13C
Pimarane, δ13C
Abietane, δ13C
ent-13-epi manoyl oxide, δ13C
2-Methyl-1-4'-methylpentyl-6-isopropylnaphthalene, δ13C
Abieta-8,11,13-triene, δ13C
Dehydroicetexane, δ13C
1,2,3,4-Tetrahydroretene, δ13C
Simonellite, δ13C
Diaromatic tricyclic totarane, δ13C
Retene, δ13C
Des-A-lupane, δ13C
Des-A-26-norlupa-5,7,9-triene, δ13C
δ13C
Schlanser, Kristen M
Diefendorf, Aaron F
West, Christopher K
Greenwood, David R
Basinger, James F
Meyer, Herbert W
Lowe, Alexander J
Naake, Hans H
Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
topic_facet carbon isotope
conifers
n-alkane
Paleogene
terpenoid
Sample ID
Latitude of event
Longitude of event
Event label
Site
Location
Epoch
AGE
Age, maximum/old
Age, minimum/young
Lithology/composition/facies
Vegetation type
Thermal maturity, hopane
Pristane/Phytane ratio
Carbon Preference Index
Terrigenous/aquatic ratio
Average chain length
Carbon, organic, total
Diterpenoids, plant-derived
Triterpenoids, plant-derived
Long-chain n-alkanes, C27-C35
Isonorpimarane, δ13C
Norpimarane, δ13C
18-Norisopimarane, δ13C
Tetracyclic diterpane, δ13C
ent-Beyerane, δ13C
13alphaH-Fichtelite, δ13C
19-Norabieta-8,11,13-triene, δ13C
19-Norabieta-4,8,11,13-tetraene, δ13C
19-Norabieta-3,8,11,13-tetraene, δ13C
18-Norabieta-8,11,13-triene, δ13C
Isopimarane, δ13C
Pimarane, δ13C
Abietane, δ13C
ent-13-epi manoyl oxide, δ13C
2-Methyl-1-4'-methylpentyl-6-isopropylnaphthalene, δ13C
Abieta-8,11,13-triene, δ13C
Dehydroicetexane, δ13C
1,2,3,4-Tetrahydroretene, δ13C
Simonellite, δ13C
Diaromatic tricyclic totarane, δ13C
Retene, δ13C
Des-A-lupane, δ13C
Des-A-26-norlupa-5,7,9-triene, δ13C
δ13C
description Paleobotanical site information, terpenoid, n-alkane, and other and biomarker quantification and carbon isotope data from sediment samples collected from North America Paleogene fossil leaf sites that extend from Colorado to the High Arctic. Sediment samples were collected laterally along fossil leaf-bearing zones. To disentangle the vegetation source of sediment n-alkanes, we measured the carbon isotope (δ13C) values of nonsteroidal triterpenoids (angiosperm biomarkers) and tricyclic diterpenoids (conifer biomarkers) to determine angiosperm and conifer end member δ13C values. Compounds were isolated using column chromatography and identified and quantified with an Agilent 7890A gas chromatograph (GC) interfaced to an Agilent 5975C quadrupole mass selective detector (MSD) and flame ionization detector (FID). Compound-specific carbon isotope analyses were performed, where possible, on n-C27 through n-C35 alkanes, diterpenoids, and triterpenoids by gas chromatograph-combustion-isotope ratio mass spectrometry ...
format Dataset
author Schlanser, Kristen M
Diefendorf, Aaron F
West, Christopher K
Greenwood, David R
Basinger, James F
Meyer, Herbert W
Lowe, Alexander J
Naake, Hans H
author_facet Schlanser, Kristen M
Diefendorf, Aaron F
West, Christopher K
Greenwood, David R
Basinger, James F
Meyer, Herbert W
Lowe, Alexander J
Naake, Hans H
author_sort Schlanser, Kristen M
title Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
title_short Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
title_full Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
title_fullStr Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
title_full_unstemmed Conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: Case studies from the Paleogene ...
title_sort conifers are a major source of sedimentary leaf wax n-alkanes when dominant on the landscape: case studies from the paleogene ...
publisher PANGAEA
publishDate 2020
url https://dx.doi.org/10.1594/pangaea.919135
https://doi.pangaea.de/10.1594/PANGAEA.919135
long_lat ENVELOPE(-65.939,-65.939,-68.664,-68.664)
geographic Arctic
Fid
geographic_facet Arctic
Fid
genre Arctic
genre_facet Arctic
op_relation https://dx.doi.org/10.1016/j.orggeochem.2020.104069
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.91913510.1016/j.orggeochem.2020.104069
_version_ 1809896970798497792