Primary succession and its driving variables – a sphere-spanning approach applied in proglacial areas in the upper Martell Valley (Eastern Italian Alps)
-
Published:2023-07-21
Issue:14
Volume:20
Page:2919-2939
-
ISSN:1726-4189
-
Container-title:Biogeosciences
-
language:en
-
Short-container-title:Biogeosciences
Author:
Ramskogler Katharina, Knoflach Bettina, Elsner Bernhard, Erschbamer Brigitta, Haas Florian, Heckmann TobiasORCID, Hofmeister FlorentinORCID, Piermattei Livia, Ressl CamilloORCID, Trautmann Svenja, Wimmer Michael H., Geitner Clemens, Stötter Johann, Tasser ErichORCID
Abstract
Abstract. Climate change and the associated glacier retreat lead to
considerable enlargement and alterations of the proglacial systems. The
colonisation of plants in this ecosystem was found to be highly dependent on
terrain age, initial site conditions and geomorphic disturbances. Although
the explanatory variables are generally well understood, there is little
knowledge on their collinearities and resulting influence on proglacial
primary succession. To develop a sphere-spanning understanding of vegetation
development, a more interdisciplinary approach was adopted. In the
proglacial areas of Fürkeleferner, Zufallferner and Langenferner (Martell
Valley, Eastern Italian Alps), in total 65 plots of 5×2 m were
installed to perform the vegetation analysis on vegetation cover, species
number and species composition. For each of those, 39 potential explanatory
variables were collected, selected through an extensive literature review.
To analyse and further avoid multicollinearities, 33 of the explanatory
variables were clustered via principal component analysis (PCA) to five
components. Subsequently, generalised additive models (GAMs) were used to
analyse the potential explanatory factors of primary succession. The results
showed that primary succession patterns were highly related to the first
component (elevation and time), the second component (solar radiation),
the third component (soil chemistry), the fifth component
(soil physics) and landforms. In summary, the analysis of all explanatory
variables together provides an overview of the most important influencing
variables and their interactions; thus it provides a basis for the debate on future
vegetation development in a changing climate.
Funder
Provincia autonoma di Bolzano - Alto Adige Austrian Science Fund
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Reference119 articles.
1. Albrecht, M., Riesen, M., and Schmid, B.: Plant-pollinator network assembly
along the chronosequence of a glacier foreland, Oikos, 119, 1610–1624,
https://doi.org/10.1111/j.1600-0706.2010.18376.x, 2010. 2. Alfredsen, G. and Høiland, K.: Succession of terrestrial macrofungi along
a deglaciation gradient at Glacier Blåisen, South Norway, Nord. J. Bot., 21, 19–37, https://doi.org/10.1111/j.1756-1051.2001.tb01335.x,
2001. 3. Andreis, C., Caccianiga, M., and Cerabolini, B.: Vegetation and
environmental factors during primary succession on glacier forelands: Some
outlines from the Italian Alps, Plant Biosyst., 135, 295–310,
https://doi.org/10.1080/11263500112331350930, 2001. 4. Anschlag, K., Tatti, D., Hellwig, N., Sartori, G., Gobat, J.-M., and Broll,
G.: Vegetation-based bioindication of humus forms in coniferous mountain
forests, J. Mt. Sci., 14, 662–673,
https://doi.org/10.1007/s11629-016-4290-y, 2017. 5. Arnold, R. W., Szabolcs, I., and Targulian, V. O.: Global soil change. Report of an IIASA-ISSS-UNEP task force on the role of
soil in global change. International Institute for Applied Systems
Analysis, Laxenburg, 1990.
|
|