Adaptive Role of Leaf Habit in Extinct Polar Forests

Fossils provide clear evidence of forests covering the Arctic and Antarctic throughout most of the past 250 million years. Ancient polar forests experienced the extreme seasonality of high latitude daylength, but flourished in a warm, temperate climate. For the past 50 years, it has been argued that...

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Published in:International Forestry Review
Main Authors: C.P. Osborne, D.L. Royer, D.J. Beerling
Format: Text
Language:English
Published: Commonwealth Forestry Association 2004
Subjects:
Online Access:https://doi.org/10.1505/ifor.6.2.181.38391
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spelling ftbioone:10.1505/ifor.6.2.181.38391 2024-06-02T07:57:28+00:00 Adaptive Role of Leaf Habit in Extinct Polar Forests C.P. Osborne D.L. Royer D.J. Beerling C.P. Osborne D.L. Royer D.J. Beerling world 2004-06-01 text/HTML https://doi.org/10.1505/ifor.6.2.181.38391 en eng Commonwealth Forestry Association doi:10.1505/ifor.6.2.181.38391 All rights reserved. https://doi.org/10.1505/ifor.6.2.181.38391 Text 2004 ftbioone https://doi.org/10.1505/ifor.6.2.181.38391 2024-05-07T01:04:12Z Fossils provide clear evidence of forests covering the Arctic and Antarctic throughout most of the past 250 million years. Ancient polar forests experienced the extreme seasonality of high latitude daylength, but flourished in a warm, temperate climate. For the past 50 years, it has been argued that deciduous trees in these ecosystems conserved carbon by avoiding the respiration required to sustain an evergreen leaf canopy during the continuous darkness of a warm winter. However, only recently have experiments been designed to test this argument by measuring the winter carbon balance of ‘living fossil’ trees in a simulated warm polar climate. Results of these experiments show clearly that the carbon cost of annually shedding leaves in deciduous trees greatly exceeds the cost of respiration for an evergreen canopy. Simulations with a mathematical model support this finding for mature forests growing across a wide latitudinal range, ending a century-long debate concerning the adaptive role of leaf habit in extinct polar forests. Text Antarc* Antarctic Arctic BioOne Online Journals Antarctic Arctic International Forestry Review 6 2 181 186
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description Fossils provide clear evidence of forests covering the Arctic and Antarctic throughout most of the past 250 million years. Ancient polar forests experienced the extreme seasonality of high latitude daylength, but flourished in a warm, temperate climate. For the past 50 years, it has been argued that deciduous trees in these ecosystems conserved carbon by avoiding the respiration required to sustain an evergreen leaf canopy during the continuous darkness of a warm winter. However, only recently have experiments been designed to test this argument by measuring the winter carbon balance of ‘living fossil’ trees in a simulated warm polar climate. Results of these experiments show clearly that the carbon cost of annually shedding leaves in deciduous trees greatly exceeds the cost of respiration for an evergreen canopy. Simulations with a mathematical model support this finding for mature forests growing across a wide latitudinal range, ending a century-long debate concerning the adaptive role of leaf habit in extinct polar forests.
author2 C.P. Osborne
D.L. Royer
D.J. Beerling
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author C.P. Osborne
D.L. Royer
D.J. Beerling
spellingShingle C.P. Osborne
D.L. Royer
D.J. Beerling
Adaptive Role of Leaf Habit in Extinct Polar Forests
author_facet C.P. Osborne
D.L. Royer
D.J. Beerling
author_sort C.P. Osborne
title Adaptive Role of Leaf Habit in Extinct Polar Forests
title_short Adaptive Role of Leaf Habit in Extinct Polar Forests
title_full Adaptive Role of Leaf Habit in Extinct Polar Forests
title_fullStr Adaptive Role of Leaf Habit in Extinct Polar Forests
title_full_unstemmed Adaptive Role of Leaf Habit in Extinct Polar Forests
title_sort adaptive role of leaf habit in extinct polar forests
publisher Commonwealth Forestry Association
publishDate 2004
url https://doi.org/10.1505/ifor.6.2.181.38391
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Arctic
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Antarctic
Arctic
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Antarctic
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