Bryophytes as indicators of climate change

Bryologist

Volumn 104, Issue 3, 2001, Pages 410-420

  Gignac, L D ^a  

^a UNIVERSITY OF ALBERTA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

BIOLOGICAL MARKER; BRYOPHYTE; CLIMATE CHANGE;

BRYOPHYTA; BRYOPHYTES; PTERIDOPHYTA;

EID: 0034790396     PISSN: 00072745     EISSN: None     Source Type: Journal    
DOI: 10.1639/0007-2745(2001)104[0410:BAIOCC]2.0.CO;2     Document Type: Review

References (23)

1. Quaternary bryophyte paleo-ecology
2. Growth under controlled conditions to explain the hierarchical distribution of the moss, Tetraphis pellucida
3. Distribution of Sphagnum species, communities, and habitats in relation to climate
4. A bioclimatic model for the distribution of Sphagnum-dominated peatlands in North America under present climatic conditions
5. The utilization of bryophytes in bioclimatic modeling: Predicted northward migration of peatlands in the Mackenzie River Basin, Canada
6. The utilization of bryophytes in bioclimatic modeling: Present distribution of peatlands in the Mackenzie River Basin, Canada
7. Sphagnum-dominated peatlands in North America since the last glacial maximum: Their occurrence and extent
8. Vascular plants as bioindicators of regional warming in Antarctica
9. Physiological ecology of mosses
10. The CCC second generation GCM and its equilibrium climate
11. Fossil mosses of North America and their significance
12. Tertiary and quaternary fossils
13. Ecotope dimensions of peatland bryophyte indicator species along gradients in the Mackenzie River Basin, Canada
14. Peatland distribution along a north-south transect in the Mackenzie River Basin in relation to climatic and environmental gradients
15. Physiological ecology
16. Bryophyte distribution patterns
17. Biogeography and conservation of bryophytes
18. Growth and production dynamics of boreal mosses over climatic, chemical and topographic gradients
19. Changes in moss-dominated wetland ecosystems
20. Climatic change in eastern North America during the past 18,000 years. Comparison of pollen data with model results