scholarly journals Diversification of Nitrogen Sources in Various Tundra Vegetation Types in the High Arctic

PLoS ONE ◽  
2015 ◽  
Vol 10 (9) ◽  
pp. e0136536 ◽  
Author(s):  
Grzegorz Skrzypek ◽  
Bronisław Wojtuń ◽  
Dorota Richter ◽  
Dariusz Jakubas ◽  
Katarzyna Wojczulanis-Jakubas ◽  
...  
2000 ◽  
Vol 14 (3) ◽  
pp. 701-713 ◽  
Author(s):  
T. R. Christensen ◽  
T. Friborg ◽  
M. Sommerkorn ◽  
J. Kaplan ◽  
L. Illeris ◽  
...  

2011 ◽  
Vol 108 (1-3) ◽  
pp. 429-445 ◽  
Author(s):  
Reiner Giesler ◽  
Camilla Esberg ◽  
Anna Lagerström ◽  
Bente J. Graae

1994 ◽  
Vol 41 (3) ◽  
pp. 306-315 ◽  
Author(s):  
Patricia M. Anderson ◽  
Patrick J. Bartlein ◽  
Linda B. Brubaker

AbstractPollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra types. These vegetation types were differentiated by combining quantitative comparisons of fossil and modern pollen assemblages with traditional, qualitative approaches for inferring past vegetation, such as the use of indicator species. Although imprecisely dated, the core probably spans at least the past 40,000 yr. A graminoid-Salix tundra dominated during the later and early portions of the glacial record. The middle glacial interval and the transition from glacial to interglacial conditions are characterized by a graminoid-Betula-Salix tundra. A Populus forest-Betula shrub tundra existed during the middle potion of this transition, being replaced in the early Holocene by a Betula-Alnus shrub tundra. The modern Picea forest-shrub tundra was established by the middle Holocene. These results suggest that the composition of modem tundra communities in northwestern Alaska developed relatively recently and that throughout much of the late Quaternary, tundra communities were unlike the predominant types found today in northern North America. Although descriptions of vegetation variations within the tundra will always be restricted by the innate taxonomic limitations of their herb-dominated pollen spectra, the application of multiple interpretive approaches improves the ability to reconstruct the historical development of this vegetation type.


2021 ◽  
Author(s):  
Katrín Björnsdóttir ◽  
Isabel C Barrio ◽  
Ingibjörg Svala Jónsdóttir

In a rapidly warming tundra, ecosystems will undergo major environmental changes which are predicted to significantly alter below–ground processes, such as decomposition of plant litter. Making use of International Tundra Experiment sites (ITEX), established approximately two decades ago, we examined long–term impacts of warming on decomposition. We used the Tea Bag Index (TBI) methodology to measure the annual mass loss (%) of two tea types as a proxy for potential decomposition rates, across five tundra vegetation types. Direct effects of warming were assessed by comparing mass loss within and outside warming manipulations. Indirect effects of warming, such as those caused by warming–induced changes in plant community composition, were assessed through the relationship between mass loss of tea and biotic and abiotic local conditions. We found positive effects of warming on decomposition, although the responses varied between vegetation and tea types. Interestingly, we found support for the indirect influence of long–term warming on decomposition through warming–induced changes in the composition of plant communities. Our findings demonstrate the complexity in decomposition responses to warming across different vegetation types and highlight the importance of long–term legacies of warming in decomposition responses across the Arctic.


2020 ◽  
Vol 724 ◽  
pp. 138304 ◽  
Author(s):  
Judith M. Sarneel ◽  
Maja K. Sundqvist ◽  
Ulf Molau ◽  
Mats P. Björkman ◽  
Juha M. Alatalo

2021 ◽  
pp. 108530
Author(s):  
Konstantin Gavazov ◽  
Alberto Canarini ◽  
Vincent E.J. Jassey ◽  
Robert Mills ◽  
Andreas Richter ◽  
...  

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