Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone

Leaf epidermal transmittance of terrestrial solar ultraviolet—B radiation (295—320 nm) was examined along a latitudinal gradient of solar UV—B radiation. In high UV—B radiation zones, e.g., equatorial and tropical regions, mean epidermal transmittance for the species examined was less than 2%. At hi...

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Published in:Ecology
Main Authors: Robberecht, Ronald, Caldwell, Martyn M., Billings, W. D.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1980
Subjects:
Online Access:http://dx.doi.org/10.2307/1937427
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spelling crwiley:10.2307/1937427 2024-04-28T08:11:12+00:00 Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone Robberecht, Ronald Caldwell, Martyn M. Billings, W. D. 1980 http://dx.doi.org/10.2307/1937427 http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F1937427 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F1937427 https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.2307/1937427 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Ecology volume 61, issue 3, page 612-619 ISSN 0012-9658 1939-9170 Ecology, Evolution, Behavior and Systematics journal-article 1980 crwiley https://doi.org/10.2307/1937427 2024-04-08T06:57:02Z Leaf epidermal transmittance of terrestrial solar ultraviolet—B radiation (295—320 nm) was examined along a latitudinal gradient of solar UV—B radiation. In high UV—B radiation zones, e.g., equatorial and tropical regions, mean epidermal transmittance for the species examined was less than 2%. At higher latitudes, mean epidermal transmittance exceeded 5%. Although this latitudinal solar UV—B gradient represents more than a seven—fold difference in daily integrated UV—B irradiance, the calculated mean effective UV—B irradiance at the mesophyll of low—latitude species is not substantially different from that of species at higher latitudes. Species in high UV—B radiation environments appear to attenuate this radiation more effectively than those in lower irradiance environments. In most cases, absorption of UV—B in the epidermis is the major parameter effecting low transmittance. Reflectance from glabrous leaves is generally less than 10%. In some species, pubescent or glaucous leaf surfaces can reflect more than 40% of the UV—B radiation incident on a horizontal leaf, although such surface characteristics do not necessarily indicate high UV—B reflectance. Under controlled conditions, epidermal transmittance in Pisum sativum L. decreased in response to UV—B irradiation. The modification of epidermal transmittance, resulting in lower UV—B irradiance at the mesophyll, may represent a mechanism of plant acclimation to UV—B radiation. Such acclimation may have occurred in several wildland species of temperate—latitude origin that have invaded high UV—B irradiance equatorial and tropical regions. Article in Journal/Newspaper Arctic Wiley Online Library Ecology 61 3 612 619
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
topic Ecology, Evolution, Behavior and Systematics
spellingShingle Ecology, Evolution, Behavior and Systematics
Robberecht, Ronald
Caldwell, Martyn M.
Billings, W. D.
Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
topic_facet Ecology, Evolution, Behavior and Systematics
description Leaf epidermal transmittance of terrestrial solar ultraviolet—B radiation (295—320 nm) was examined along a latitudinal gradient of solar UV—B radiation. In high UV—B radiation zones, e.g., equatorial and tropical regions, mean epidermal transmittance for the species examined was less than 2%. At higher latitudes, mean epidermal transmittance exceeded 5%. Although this latitudinal solar UV—B gradient represents more than a seven—fold difference in daily integrated UV—B irradiance, the calculated mean effective UV—B irradiance at the mesophyll of low—latitude species is not substantially different from that of species at higher latitudes. Species in high UV—B radiation environments appear to attenuate this radiation more effectively than those in lower irradiance environments. In most cases, absorption of UV—B in the epidermis is the major parameter effecting low transmittance. Reflectance from glabrous leaves is generally less than 10%. In some species, pubescent or glaucous leaf surfaces can reflect more than 40% of the UV—B radiation incident on a horizontal leaf, although such surface characteristics do not necessarily indicate high UV—B reflectance. Under controlled conditions, epidermal transmittance in Pisum sativum L. decreased in response to UV—B irradiation. The modification of epidermal transmittance, resulting in lower UV—B irradiance at the mesophyll, may represent a mechanism of plant acclimation to UV—B radiation. Such acclimation may have occurred in several wildland species of temperate—latitude origin that have invaded high UV—B irradiance equatorial and tropical regions.
format Article in Journal/Newspaper
author Robberecht, Ronald
Caldwell, Martyn M.
Billings, W. D.
author_facet Robberecht, Ronald
Caldwell, Martyn M.
Billings, W. D.
author_sort Robberecht, Ronald
title Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
title_short Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
title_full Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
title_fullStr Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
title_full_unstemmed Leaf Ultraviolet Optical Properties Along a Latitudinal Gradient in the Arctic‐Alpine Life Zone
title_sort leaf ultraviolet optical properties along a latitudinal gradient in the arctic‐alpine life zone
publisher Wiley
publishDate 1980
url http://dx.doi.org/10.2307/1937427
http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F1937427
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F1937427
https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.2307/1937427
genre Arctic
genre_facet Arctic
op_source Ecology
volume 61, issue 3, page 612-619
ISSN 0012-9658 1939-9170
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.2307/1937427
container_title Ecology
container_volume 61
container_issue 3
container_start_page 612
op_container_end_page 619
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