Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland
The hydrogen isotopic composition (δ²H values) of plant waxes preserved in the sedimentary record is a useful proxy for past hydroclimate, but a number of known biological and environmental factors can confound the climate signal this proxy records. High-latitude ecology and environmental conditio...
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Online Access: | https://doi.org/10.1016/j.gca.2020.07.027 |
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ftcaltechauth:oai:authors.library.caltech.edu:9ekqb-4pj78 2024-06-23T07:50:06+00:00 Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland Dion-Kirschner, Hannah McFarlin, Jamie M. Masterson, Andrew L. Axford, Yarrow Osburn, Magdalena R. 2020-10-01 https://doi.org/10.1016/j.gca.2020.07.027 unknown Elsevier https://doi.org/10.1016/j.gca.2020.07.027 oai:authors.library.caltech.edu:9ekqb-4pj78 eprintid:105358 resolverid:CaltechAUTHORS:20200911-133139424 info:eu-repo/semantics/openAccess Other Geochimica et Cosmochimica Acta, 286, 336-354, (2020-10-01) Compound-specific hydrogen isotopes Compound-specific carbon isotopes Leaf waxes Paleohydrology Paleoclimate Arctic lakes Greenland Kangerlussuaq info:eu-repo/semantics/article 2020 ftcaltechauth https://doi.org/10.1016/j.gca.2020.07.027 2024-06-12T05:40:57Z The hydrogen isotopic composition (δ²H values) of plant waxes preserved in the sedimentary record is a useful proxy for past hydroclimate, but a number of known biological and environmental factors can confound the climate signal this proxy records. High-latitude ecology and environmental conditions differ from those of the better-studied low latitudes, and the influence of arctic conditions on factors that affect δ²H records of climate is poorly constrained. Direct observations of arctic plant waxes and their δ²H values, particularly from aquatic plants, are very limited. Here we present a study of n-alkane and n-alkanoic acid homologue distributions, δ²H values, and δ¹³C values from west Greenland, including measurements of terrestrial and aquatic plants, algae, and Nostoc (colonial cyanobacteria). By examining samples collected from the same region and season, we focus on climate-independent factors that may affect the δ²H values of sedimentary plant waxes. We observe that the average abundance of leaf n-alkyl lipids (Câ‚‚â‚€-C₃â‚) in common terrestrial plants from this region exceeds that in aquatic sources by up to 30×. We also note weaker source specificity in n-alkanoic acids than in n-alkanes. A comparison of these data with surface sedimentary plant waxes from a lake within the study area, previously reported by McFarlin et al. (2019), indicates that at this site both mid-chain and long-chain sedimentary waxes are likely to derive from dominantly terrestrial sources, particularly biased towards the genus Salix. Abundance-weighted isotope data reveal that while terrestrial plants show taxonomic trends in δ²H values, the amplitude of these trends is unlikely to exceed the error of the proxy (the standard deviation on calculated ε_(app)). n-Alkane ε_(app) values are more variable in aquatic than in terrestrial sources, with median values ranging from −115‰ in n-C₃₠to −143‰ in n-Câ‚‚â‚. However, because sedimentary waxes at our study site are most similar to terrestrial ... Article in Journal/Newspaper Arctic Greenland Kangerlussuaq Caltech Authors (California Institute of Technology) Arctic Greenland Kangerlussuaq ENVELOPE(-55.633,-55.633,72.633,72.633) Geochimica et Cosmochimica Acta 286 336 354 |
institution |
Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
topic |
Compound-specific hydrogen isotopes Compound-specific carbon isotopes Leaf waxes Paleohydrology Paleoclimate Arctic lakes Greenland Kangerlussuaq |
spellingShingle |
Compound-specific hydrogen isotopes Compound-specific carbon isotopes Leaf waxes Paleohydrology Paleoclimate Arctic lakes Greenland Kangerlussuaq Dion-Kirschner, Hannah McFarlin, Jamie M. Masterson, Andrew L. Axford, Yarrow Osburn, Magdalena R. Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
topic_facet |
Compound-specific hydrogen isotopes Compound-specific carbon isotopes Leaf waxes Paleohydrology Paleoclimate Arctic lakes Greenland Kangerlussuaq |
description |
The hydrogen isotopic composition (δ²H values) of plant waxes preserved in the sedimentary record is a useful proxy for past hydroclimate, but a number of known biological and environmental factors can confound the climate signal this proxy records. High-latitude ecology and environmental conditions differ from those of the better-studied low latitudes, and the influence of arctic conditions on factors that affect δ²H records of climate is poorly constrained. Direct observations of arctic plant waxes and their δ²H values, particularly from aquatic plants, are very limited. Here we present a study of n-alkane and n-alkanoic acid homologue distributions, δ²H values, and δ¹³C values from west Greenland, including measurements of terrestrial and aquatic plants, algae, and Nostoc (colonial cyanobacteria). By examining samples collected from the same region and season, we focus on climate-independent factors that may affect the δ²H values of sedimentary plant waxes. We observe that the average abundance of leaf n-alkyl lipids (Câ‚‚â‚€-C₃â‚) in common terrestrial plants from this region exceeds that in aquatic sources by up to 30×. We also note weaker source specificity in n-alkanoic acids than in n-alkanes. A comparison of these data with surface sedimentary plant waxes from a lake within the study area, previously reported by McFarlin et al. (2019), indicates that at this site both mid-chain and long-chain sedimentary waxes are likely to derive from dominantly terrestrial sources, particularly biased towards the genus Salix. Abundance-weighted isotope data reveal that while terrestrial plants show taxonomic trends in δ²H values, the amplitude of these trends is unlikely to exceed the error of the proxy (the standard deviation on calculated ε_(app)). n-Alkane ε_(app) values are more variable in aquatic than in terrestrial sources, with median values ranging from −115‰ in n-C₃₠to −143‰ in n-Câ‚‚â‚. However, because sedimentary waxes at our study site are most similar to terrestrial ... |
format |
Article in Journal/Newspaper |
author |
Dion-Kirschner, Hannah McFarlin, Jamie M. Masterson, Andrew L. Axford, Yarrow Osburn, Magdalena R. |
author_facet |
Dion-Kirschner, Hannah McFarlin, Jamie M. Masterson, Andrew L. Axford, Yarrow Osburn, Magdalena R. |
author_sort |
Dion-Kirschner, Hannah |
title |
Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
title_short |
Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
title_full |
Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
title_fullStr |
Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
title_full_unstemmed |
Modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west Greenland |
title_sort |
modern constraints on the sources and climate signals recorded by sedimentary plant waxes in west greenland |
publisher |
Elsevier |
publishDate |
2020 |
url |
https://doi.org/10.1016/j.gca.2020.07.027 |
long_lat |
ENVELOPE(-55.633,-55.633,72.633,72.633) |
geographic |
Arctic Greenland Kangerlussuaq |
geographic_facet |
Arctic Greenland Kangerlussuaq |
genre |
Arctic Greenland Kangerlussuaq |
genre_facet |
Arctic Greenland Kangerlussuaq |
op_source |
Geochimica et Cosmochimica Acta, 286, 336-354, (2020-10-01) |
op_relation |
https://doi.org/10.1016/j.gca.2020.07.027 oai:authors.library.caltech.edu:9ekqb-4pj78 eprintid:105358 resolverid:CaltechAUTHORS:20200911-133139424 |
op_rights |
info:eu-repo/semantics/openAccess Other |
op_doi |
https://doi.org/10.1016/j.gca.2020.07.027 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
286 |
container_start_page |
336 |
op_container_end_page |
354 |
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1802640867732750336 |