Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska

In primary succession following deglaciation at Glacier Bay, Alaska, we tested the hypothesis that the major effect of initial nitrogen—fixing colonizers is to facilitate establishment of late—successional dominants and that other possible causes of successional change (e.g., life history factors go...

Full description

Bibliographic Details
Published in:Ecological Monographs
Main Authors: Chapin, F. Stuart, Walker, Lawrence R., Fastie, Christopher L., Sharman, Lewis C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1994
Subjects:
Online Access:http://dx.doi.org/10.2307/2937039
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F2937039
https://onlinelibrary.wiley.com/doi/pdf/10.2307/2937039
https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.2307/2937039
id crwiley:10.2307/2937039
record_format openpolar
spelling crwiley:10.2307/2937039 2024-10-20T14:08:50+00:00 Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska Chapin, F. Stuart Walker, Lawrence R. Fastie, Christopher L. Sharman, Lewis C. 1994 http://dx.doi.org/10.2307/2937039 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F2937039 https://onlinelibrary.wiley.com/doi/pdf/10.2307/2937039 https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.2307/2937039 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Ecological Monographs volume 64, issue 2, page 149-175 ISSN 0012-9615 1557-7015 journal-article 1994 crwiley https://doi.org/10.2307/2937039 2024-09-23T04:37:10Z In primary succession following deglaciation at Glacier Bay, Alaska, we tested the hypothesis that the major effect of initial nitrogen—fixing colonizers is to facilitate establishment of late—successional dominants and that other possible causes of successional change (e.g., life history factors governing seed rain and competitive interactions among species) need not be invoked. Environment changed dramatically through the first 200 yr of succession. Soil organic matter increased 10—fold in the upper mineral soil with corresponding increases in soil moisture, total nitrogen (N), and capacity to support plant growth and declines in bulk density, pH, and total phosphorus (P). Plant growth in pioneer soils tended to be simultaneously limited by both N and P, as well as by unknown factors (perhaps lack of mycorrhizae), whereas only P limited growth in older soils. Light availability to seedlings declined through succession. Early—successional species (Epilobium latifolium, Dryas drummondii) had smaller seeds, younger age at first reproduction, shorter life—span, and shorter height at maturity than did mid—successional (alder, Alnus sinuata) and late—successional species (sitka spruce, Picea sitchensis). Seed rain of alder and spruce was negligible in the pioneer stage, increased prior to the stage in which a species was dominant, and was greatest in the stage in which a species dominated. Vegetation in each successional stage inhibited germination and initial establishment of sown alder and spruce seeds (except a tendency of the "black—crust") algal/microbial community in the pioneer stage to enhance survivorship). Removal of the surface litter layer generally enhanced germination and survivorship, particularly of alder. Comparisons of germination in the greenhouse and the field indicated that climatic or indirect vegetation effects (e.g., differential seed predation) and allelopathy also reduced germination and establishment in vegetated communities. Naturally occurring spruce seedlings grew most rapidly in the ... Article in Journal/Newspaper glacier Alaska Wiley Online Library Glacier Bay Ecological Monographs 64 2 149 175
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description In primary succession following deglaciation at Glacier Bay, Alaska, we tested the hypothesis that the major effect of initial nitrogen—fixing colonizers is to facilitate establishment of late—successional dominants and that other possible causes of successional change (e.g., life history factors governing seed rain and competitive interactions among species) need not be invoked. Environment changed dramatically through the first 200 yr of succession. Soil organic matter increased 10—fold in the upper mineral soil with corresponding increases in soil moisture, total nitrogen (N), and capacity to support plant growth and declines in bulk density, pH, and total phosphorus (P). Plant growth in pioneer soils tended to be simultaneously limited by both N and P, as well as by unknown factors (perhaps lack of mycorrhizae), whereas only P limited growth in older soils. Light availability to seedlings declined through succession. Early—successional species (Epilobium latifolium, Dryas drummondii) had smaller seeds, younger age at first reproduction, shorter life—span, and shorter height at maturity than did mid—successional (alder, Alnus sinuata) and late—successional species (sitka spruce, Picea sitchensis). Seed rain of alder and spruce was negligible in the pioneer stage, increased prior to the stage in which a species was dominant, and was greatest in the stage in which a species dominated. Vegetation in each successional stage inhibited germination and initial establishment of sown alder and spruce seeds (except a tendency of the "black—crust") algal/microbial community in the pioneer stage to enhance survivorship). Removal of the surface litter layer generally enhanced germination and survivorship, particularly of alder. Comparisons of germination in the greenhouse and the field indicated that climatic or indirect vegetation effects (e.g., differential seed predation) and allelopathy also reduced germination and establishment in vegetated communities. Naturally occurring spruce seedlings grew most rapidly in the ...
format Article in Journal/Newspaper
author Chapin, F. Stuart
Walker, Lawrence R.
Fastie, Christopher L.
Sharman, Lewis C.
spellingShingle Chapin, F. Stuart
Walker, Lawrence R.
Fastie, Christopher L.
Sharman, Lewis C.
Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
author_facet Chapin, F. Stuart
Walker, Lawrence R.
Fastie, Christopher L.
Sharman, Lewis C.
author_sort Chapin, F. Stuart
title Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
title_short Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
title_full Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
title_fullStr Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
title_full_unstemmed Mechanisms of Primary Succession Following Deglaciation at Glacier Bay, Alaska
title_sort mechanisms of primary succession following deglaciation at glacier bay, alaska
publisher Wiley
publishDate 1994
url http://dx.doi.org/10.2307/2937039
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.2307%2F2937039
https://onlinelibrary.wiley.com/doi/pdf/10.2307/2937039
https://esajournals.onlinelibrary.wiley.com/doi/pdf/10.2307/2937039
geographic Glacier Bay
geographic_facet Glacier Bay
genre glacier
Alaska
genre_facet glacier
Alaska
op_source Ecological Monographs
volume 64, issue 2, page 149-175
ISSN 0012-9615 1557-7015
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.2307/2937039
container_title Ecological Monographs
container_volume 64
container_issue 2
container_start_page 149
op_container_end_page 175
_version_ 1813448037554454528