Diversity in Primary Succession: The Chronosequence of a Glacier Foreland

2019 ◽  
pp. 177-190 ◽  
Author(s):  
Rüdiger Kaufmann ◽  
Corinna Raffl
2012 ◽  
Vol 44 (1) ◽  
pp. 2-15 ◽  
Author(s):  
Anders Thon Bråten ◽  
Daniel Flø ◽  
Sigmund Hågvar ◽  
Oddvar Hanssen ◽  
Christian E. Mong ◽  
...  

2006 ◽  
Vol 72 (9) ◽  
pp. 5957-5962 ◽  
Author(s):  
Ellen Kandeler ◽  
Kathrin Deiglmayr ◽  
Dagmar Tscherko ◽  
David Bru ◽  
Laurent Philippot

ABSTRACT Quantitative PCR of denitrification genes encoding the nitrate, nitrite, and nitrous oxide reductases was used to study denitrifiers across a glacier foreland. Environmental samples collected at different distances from a receding glacier contained amounts of 16S rRNA target molecules ranging from 4.9 � 105 to 8.9 � 105 copies per nanogram of DNA but smaller amounts of narG, nirK, and nosZ target molecules. Thus, numbers of narG, nirK, nirS, and nosZ copies per nanogram of DNA ranged from 2.1 � 103 to 2.6 � 104, 7.4 � 102 to 1.4 � 103, 2.5 � 102 to 6.4 � 103, and 1.2 � 103 to 5.5 � 103, respectively. The densities of 16S rRNA genes per gram of soil increased with progressing soil development. The densities as well as relative abundances of different denitrification genes provide evidence that different denitrifier communities develop under primary succession: higher percentages of narG and nirS versus 16S rRNA genes were observed in the early stage of primary succession, while the percentages of nirK and nosZ genes showed no significant increase or decrease with soil age. Statistical analyses revealed that the amount of organic substances was the most important factor in the abundance of eubacteria as well as of nirK and nosZ communities, and copy numbers of these two genes were the most important drivers changing the denitrifying community along the chronosequence. This study yields an initial insight into the ecology of bacteria carrying genes for the denitrification pathway in a newly developing alpine environment.


Alpine Botany ◽  
2016 ◽  
Vol 126 (2) ◽  
pp. 105-117 ◽  
Author(s):  
Katharina Schumann ◽  
Susanne Gewolf ◽  
Oliver Tackenberg

2020 ◽  
Author(s):  
Stefan Haselberger ◽  
Lisa Maria Ohler ◽  
Robert R. Junker ◽  
Jan-Christoph Otto ◽  
Sabine Kraushaar

<p>Landscape change is an interplay of abiotic and biotic processes with bi-directional and interwoven relationships. Glacier foreland areas can act as open-air laboratory to observe biogeomorphic interactions. Paraglacial adjustment establishes initial conditions for ecological succession and requires constant feedbacks between plants and landscapes. Frequency and magnitude of geomorphic processes and functional composition and abundance of plants govern these responses. Up to now, biogeomorphic studies have mainly focused on the qualitative description of the relationship between biotic and abiotic processes. However, in order to test biogeomorphic concepts, it is necessary to jointly quantify (i) geomorphic process rates as a function of vegetation and (ii) successional development as a function of geomorphic conditions.</p><p>The proglacial area of the Gepatschferner (Kaunertal) in the crystalline Central Eastern Alps presents a showcase environment to investigate these interactions as the retreating glacier and highly active slope processes provide the ground for different stages of ecological succession and promotes high rates of sediment reworking within the proglacial deposits.</p><p>In this particular study, we investigate small-scale biogeomorphic interactions at 30 test sites of 2*3m size. Experimental plots are established on slopes along an ecological succession gradient that reflect different stages of erosion-vegetation interaction. To cover the abiotic condition for the plot sites morphometric characteristics and edaphic variables were determined. In order to quantify abiotic process rates, we use mechanical measurements (i.e. erosion plots) to determine sediment yield and to measure the effect of vegetation on particle size distribution. Relative Dating, historical image analysis and knowledge of glacial retreat helped to estimate time since last perturbation. A detailed vegetation survey was carried out to capture biotic conditions at the sites. Species distribution and abundance at each site, as well as plant functional types provide information on successional stage and functional diversity.</p><p>This data set provides a vital opportunity to test conceptual models on biogeomorphic succession in glacier forelands and to evaluate the bi-directional influence of primary succession on small-scale sediment transport and vice versa.</p>


2005 ◽  
Vol 7 (3) ◽  
pp. 337-347 ◽  
Author(s):  
Graeme W. Nicol ◽  
Dagmar Tscherko ◽  
T. Martin Embley ◽  
James I. Prosser

2010 ◽  
Vol 186 (2) ◽  
pp. 451-460 ◽  
Author(s):  
Shinpei Yoshitake ◽  
Masaki Uchida ◽  
Hiroshi Koizumi ◽  
Hiroshi Kanda ◽  
Takayuki Nakatsubo

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