Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest

Abundant fossil plant remains are preserved in the high-latitude late Paleocene Iceberg Bay Formation on Ellesmere Island, Nunavut, Canada. Intact leaf litter lenses and permineralized, in situ logs and stumps offer for the first time an opportunity to determine the structure, biomass, and productiv...

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Published in:Proceedings of the Academy of Natural Sciences of Philadelphia
Main Authors: Christopher J. Williams, Ben A. LePage, Arthur H. Johnson, David R. Vann
Format: Text
Language:English
Published: The Academy of Natural Sciences of Philadelphia 2009
Subjects:
Online Access:https://doi.org/10.1635/053.158.0106
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spelling ftbioone:10.1635/053.158.0106 2023-07-30T04:02:09+02:00 Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest Christopher J. Williams Ben A. LePage Arthur H. Johnson David R. Vann Christopher J. Williams Ben A. LePage Arthur H. Johnson David R. Vann world 2009-04-01 text/HTML https://doi.org/10.1635/053.158.0106 en eng The Academy of Natural Sciences of Philadelphia doi:10.1635/053.158.0106 All rights reserved. https://doi.org/10.1635/053.158.0106 Text 2009 ftbioone https://doi.org/10.1635/053.158.0106 2023-07-09T10:27:17Z Abundant fossil plant remains are preserved in the high-latitude late Paleocene Iceberg Bay Formation on Ellesmere Island, Nunavut, Canada. Intact leaf litter lenses and permineralized, in situ logs and stumps offer for the first time an opportunity to determine the structure, biomass, and productivity of a redwood-dominated forest that grew in the polar regions of Nunavut (paleolatitude 75–80° N). Well-preserved fossil tree trunks were excavated to develop equations that describe the height, structure, and mass of the aboveground components of late Paleocene-age (approximately 55.8 to 58.7 million years old) Metasequoia (redwoods) trees. We then combined those data with measurements of the in situ stumps to determine the structure, biomass, and productivity of this polar fossil forest. The height of the canopy trees in the forest was calculated to be 32 ± 2 m. Abundant branch stubs that represent the remnants of living branches were found on a wide range of stem sizes including larger logs from the lower portions of the fossil trees indicating a relatively deep canopy. The branch lengths predicted from allometric relationships developed on modern Metasequoia trees are consistent with the stump spacing measured at Stenkul Fiord. The stem volume equaled 1,632 m3 ha-1 and stem biomass was a minimum of 490 Mg ha-1. Recovery of an incomplete treetop with exposed branch stubs enabled us to make minimum estimates of branch wood and foliar biomass using allometric equations derived from extant Metasequoia glyptostroboides trees in Japan. Estimated stand-level branch biomass was at most 19 Mg ha-1 and standing foliar biomass was estimated to be a maximum of 4 Mg ha-1. We adjusted the derived stemwood biomass estimates to account for a potential bias against sapwood and bark preservation. This adjustment increased our stemwood biomass estimates by 17% to 576 Mg ha-1. Using the annual ring widths of the tree stems, the reconstructed parabolic stems, and wood density of modern Metasequoia, we calculated the annual wood ... Text Arctic Ellesmere Island Iceberg Bay Iceberg* Nunavut BioOne Online Journals Arctic Canada Ellesmere Island Iceberg Bay ENVELOPE(69.177,69.177,-49.559,-49.559) Nunavut Stump ENVELOPE(-153.167,-153.167,-86.183,-86.183) The Stump ENVELOPE(-58.161,-58.161,-62.097,-62.097) Proceedings of the Academy of Natural Sciences of Philadelphia 158 1 107 127
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language English
description Abundant fossil plant remains are preserved in the high-latitude late Paleocene Iceberg Bay Formation on Ellesmere Island, Nunavut, Canada. Intact leaf litter lenses and permineralized, in situ logs and stumps offer for the first time an opportunity to determine the structure, biomass, and productivity of a redwood-dominated forest that grew in the polar regions of Nunavut (paleolatitude 75–80° N). Well-preserved fossil tree trunks were excavated to develop equations that describe the height, structure, and mass of the aboveground components of late Paleocene-age (approximately 55.8 to 58.7 million years old) Metasequoia (redwoods) trees. We then combined those data with measurements of the in situ stumps to determine the structure, biomass, and productivity of this polar fossil forest. The height of the canopy trees in the forest was calculated to be 32 ± 2 m. Abundant branch stubs that represent the remnants of living branches were found on a wide range of stem sizes including larger logs from the lower portions of the fossil trees indicating a relatively deep canopy. The branch lengths predicted from allometric relationships developed on modern Metasequoia trees are consistent with the stump spacing measured at Stenkul Fiord. The stem volume equaled 1,632 m3 ha-1 and stem biomass was a minimum of 490 Mg ha-1. Recovery of an incomplete treetop with exposed branch stubs enabled us to make minimum estimates of branch wood and foliar biomass using allometric equations derived from extant Metasequoia glyptostroboides trees in Japan. Estimated stand-level branch biomass was at most 19 Mg ha-1 and standing foliar biomass was estimated to be a maximum of 4 Mg ha-1. We adjusted the derived stemwood biomass estimates to account for a potential bias against sapwood and bark preservation. This adjustment increased our stemwood biomass estimates by 17% to 576 Mg ha-1. Using the annual ring widths of the tree stems, the reconstructed parabolic stems, and wood density of modern Metasequoia, we calculated the annual wood ...
author2 Christopher J. Williams
Ben A. LePage
Arthur H. Johnson
David R. Vann
format Text
author Christopher J. Williams
Ben A. LePage
Arthur H. Johnson
David R. Vann
spellingShingle Christopher J. Williams
Ben A. LePage
Arthur H. Johnson
David R. Vann
Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
author_facet Christopher J. Williams
Ben A. LePage
Arthur H. Johnson
David R. Vann
author_sort Christopher J. Williams
title Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
title_short Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
title_full Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
title_fullStr Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
title_full_unstemmed Structure, Biomass, and Productivity of a Late Paleocene Arctic Forest
title_sort structure, biomass, and productivity of a late paleocene arctic forest
publisher The Academy of Natural Sciences of Philadelphia
publishDate 2009
url https://doi.org/10.1635/053.158.0106
op_coverage world
long_lat ENVELOPE(69.177,69.177,-49.559,-49.559)
ENVELOPE(-153.167,-153.167,-86.183,-86.183)
ENVELOPE(-58.161,-58.161,-62.097,-62.097)
geographic Arctic
Canada
Ellesmere Island
Iceberg Bay
Nunavut
Stump
The Stump
geographic_facet Arctic
Canada
Ellesmere Island
Iceberg Bay
Nunavut
Stump
The Stump
genre Arctic
Ellesmere Island
Iceberg Bay
Iceberg*
Nunavut
genre_facet Arctic
Ellesmere Island
Iceberg Bay
Iceberg*
Nunavut
op_source https://doi.org/10.1635/053.158.0106
op_relation doi:10.1635/053.158.0106
op_rights All rights reserved.
op_doi https://doi.org/10.1635/053.158.0106
container_title Proceedings of the Academy of Natural Sciences of Philadelphia
container_volume 158
container_issue 1
container_start_page 107
op_container_end_page 127
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