Predicting distribution changes of a mire ecosystem under future climates

2014 ◽  
Vol 20 (4) ◽  
pp. 440-454 ◽  
Author(s):  
David A. Keith ◽  
Jane Elith ◽  
Christopher C. Simpson
Keyword(s):  
2008 ◽  
Vol 112 (5) ◽  
pp. 1956-1968 ◽  
Author(s):  
L.T. Waser ◽  
E. Baltsavias ◽  
K. Ecker ◽  
H. Eisenbeiss ◽  
E. Feldmeyer-Christe ◽  
...  

2013 ◽  
Vol 40 (3) ◽  
pp. 177-186
Author(s):  
Jacek Chodorowski ◽  
Andrzej Plak ◽  
Irena Pidek ◽  
Radosław Dobrowolski

AbstractMulti-proxy analysis (sedimentological, palaeobotanical, geochemical data and results of radiocarbon dating) of the biogenic sediments from a small mire ecosystem in the Sandomierz Basin (SE Poland) is presented. The ecosystem contains a full hydroseral sequence from minerotrophic to ombrotrophic wetland. It is one of the few sites in this region which is so thoroughly investigated in terms of the palaeoenvironmental record. Changes in the water supply of the mire area, and consequently the changes in the plant and sediment succession, were well correlated with the regional tendencies in precipitation and temperature during the Late Glacial/Holocene transition and in the Holocene. Human impact is very well recorded in pollen diagram from the Subboreal period.


2020 ◽  
Author(s):  
Patrik Vestin ◽  
Per Weslien ◽  
Marcus Wallin ◽  
David Bastviken ◽  
Natascha Kljun ◽  
...  

<p>We present the Net Ecosystem Carbon Balance (NECB) of a Northern mire ecosystem for the period 2016-2019. The Mycklemossen peatland is located in the hemi-boreal region in the Southwestern part of Sweden and is classified as a fen with bog-like vegetation. The NECB was determined from eddy covariance (EC) measurements of carbon dioxide (CO<sub>2</sub>) and methane (CH<sub>4</sub>) and continuous water discharge measurements with biweekly measurements of dissolved organic carbon (DOC), dissolved inorganic carbon (DIC) and dissolved CH<sub>4</sub>. <br>We focus on the carbon dynamics of the Mycklemossen ecosystem during summer droughts and on its recovery during normal years. During 2016-2018, the annual precipitation was lower than the 30-year average while 2019 was a normal year in terms of weather conditions. 2018 sticks out as an extreme year with a severe drought and unusually high air temperature at Mycklemossen, as was the case in much of Northern and Central Europe.<br>The EC results indicate that Mycklemossen lost carbon during 2016-2018. While CH<sub>4</sub> emissions decreased, the mire became a strong source of CO<sub>2</sub> these years, especially 2018. There were also large losses of DOC during this period, which were further enhanced during 2019.</p>


2020 ◽  
Vol 280 ◽  
pp. 107783 ◽  
Author(s):  
Peter Levy ◽  
Julia Drewer ◽  
Mathilde Jammet ◽  
Sarah Leeson ◽  
Thomas Friborg ◽  
...  

Author(s):  
Teemu Tahvanainen ◽  
Lucie Bland ◽  
Lars Granlund ◽  
Urban Gunnarsson ◽  
David Keith ◽  
...  

2002 ◽  
Vol 17 (5) ◽  
pp. 601-613 ◽  
Author(s):  
Kazuo Yabe ◽  
Takatoshi Nakamura

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