Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene
Novel fire regimes are expected in many boreal regions, and it is unclear how biogeochemical cycles will respond. We leverage fire and vegetation records from a highly flammable ecoregion in Alaska and present new lake-sediment analyses to examine biogeochemical responses to fire over the past 5300...
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ftdryad:oai:v1.datadryad.org:10255/dryad.217664 2023-05-15T17:57:23+02:00 Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene Chipman, Melissa L. Hu, Feng Sheng Yukon Flats Alaska 5300 calibrated years BP 2019-08-09T13:09:54Z http://hdl.handle.net/10255/dryad.217664 https://doi.org/10.5061/dryad.440rk01 unknown doi:10.5061/dryad.440rk01/1 doi:10.1098/rsbl.2019.0390 doi:10.5061/dryad.440rk01 Chipman ML, Hu FS (2019) Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene. Biology Letters 15(8): 20190390. http://hdl.handle.net/10255/dryad.217664 boreal fires nitrogen carbon δ15N δ13C C:N ecological resilience Article 2019 ftdryad https://doi.org/10.5061/dryad.440rk01 https://doi.org/10.5061/dryad.440rk01/1 https://doi.org/10.1098/rsbl.2019.0390 2020-01-01T16:29:12Z Novel fire regimes are expected in many boreal regions, and it is unclear how biogeochemical cycles will respond. We leverage fire and vegetation records from a highly flammable ecoregion in Alaska and present new lake-sediment analyses to examine biogeochemical responses to fire over the past 5300 years. No significant difference exists in δ13C, %C, %N, C:N, or magnetic susceptibility between pre-fire, post-fire, and fire samples. However, δ15N is related to the timing relative to fire (Χ2=19.73, p<0.0001), with higher values for fire-decade samples (3.2±0.3‰) than pre-fire (2.4±0.2‰) and post-fire (2.2±0.1‰) samples. Sediment δ15N increased gradually from 1.8±0.6‰ to 3.2±0.2‰ over the late Holocene, probably as a result of terrestrial-ecosystem development. Elevated δ15N in fire decades likely reflects enhanced terrestrial nitrification and/or deeper permafrost-thaw depths immediately following fire. Similar δ15N values before and after fire decades suggest that N cycling in this lowland-boreal watershed was resilient to fire disturbance. However, this resilience may diminish as boreal ecosystems approach climate-driven thresholds of vegetation structure, permafrost thaw, and fire. Article in Journal/Newspaper permafrost Alaska Yukon Dryad Digital Repository (Duke University) Yukon New Lake ENVELOPE(-109.468,-109.468,62.684,62.684) |
institution |
Open Polar |
collection |
Dryad Digital Repository (Duke University) |
op_collection_id |
ftdryad |
language |
unknown |
topic |
boreal fires nitrogen carbon δ15N δ13C C:N ecological resilience |
spellingShingle |
boreal fires nitrogen carbon δ15N δ13C C:N ecological resilience Chipman, Melissa L. Hu, Feng Sheng Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
topic_facet |
boreal fires nitrogen carbon δ15N δ13C C:N ecological resilience |
description |
Novel fire regimes are expected in many boreal regions, and it is unclear how biogeochemical cycles will respond. We leverage fire and vegetation records from a highly flammable ecoregion in Alaska and present new lake-sediment analyses to examine biogeochemical responses to fire over the past 5300 years. No significant difference exists in δ13C, %C, %N, C:N, or magnetic susceptibility between pre-fire, post-fire, and fire samples. However, δ15N is related to the timing relative to fire (Χ2=19.73, p<0.0001), with higher values for fire-decade samples (3.2±0.3‰) than pre-fire (2.4±0.2‰) and post-fire (2.2±0.1‰) samples. Sediment δ15N increased gradually from 1.8±0.6‰ to 3.2±0.2‰ over the late Holocene, probably as a result of terrestrial-ecosystem development. Elevated δ15N in fire decades likely reflects enhanced terrestrial nitrification and/or deeper permafrost-thaw depths immediately following fire. Similar δ15N values before and after fire decades suggest that N cycling in this lowland-boreal watershed was resilient to fire disturbance. However, this resilience may diminish as boreal ecosystems approach climate-driven thresholds of vegetation structure, permafrost thaw, and fire. |
format |
Article in Journal/Newspaper |
author |
Chipman, Melissa L. Hu, Feng Sheng |
author_facet |
Chipman, Melissa L. Hu, Feng Sheng |
author_sort |
Chipman, Melissa L. |
title |
Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
title_short |
Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
title_full |
Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
title_fullStr |
Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
title_full_unstemmed |
Data from: Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene |
title_sort |
data from: resilience of lake biogeochemistry to boreal-forest wildfires during the late holocene |
publishDate |
2019 |
url |
http://hdl.handle.net/10255/dryad.217664 https://doi.org/10.5061/dryad.440rk01 |
op_coverage |
Yukon Flats Alaska 5300 calibrated years BP |
long_lat |
ENVELOPE(-109.468,-109.468,62.684,62.684) |
geographic |
Yukon New Lake |
geographic_facet |
Yukon New Lake |
genre |
permafrost Alaska Yukon |
genre_facet |
permafrost Alaska Yukon |
op_relation |
doi:10.5061/dryad.440rk01/1 doi:10.1098/rsbl.2019.0390 doi:10.5061/dryad.440rk01 Chipman ML, Hu FS (2019) Resilience of lake biogeochemistry to boreal-forest wildfires during the late Holocene. Biology Letters 15(8): 20190390. http://hdl.handle.net/10255/dryad.217664 |
op_doi |
https://doi.org/10.5061/dryad.440rk01 https://doi.org/10.5061/dryad.440rk01/1 https://doi.org/10.1098/rsbl.2019.0390 |
_version_ |
1766165795115630592 |