Effect of hydrogeomorphic setting on calcareous fen hydrology

2018 ◽  
Vol 32 (11) ◽  
pp. 1695-1708 ◽  
Author(s):  
Tim P. Duval ◽  
James Michael Waddington
Keyword(s):  
2020 ◽  
Vol 55 (3) ◽  
pp. 151-162
Author(s):  
Danuta Urban ◽  
Joanna Sender ◽  
Ewelina Tokarz ◽  
Andrzej Różycki

AbstractIn view of the sensitivity of Liparis loeselii to changes in habitat conditions, we carried out a study with the aim to monitor population numbers, identify the individual features of the Liparis loeselii population, analyse habitat conditions, identify threats and propose conservation measures to preserve the species. The investigations were conducted in seven unmanaged objects located in three Natura 2000 areas in eastern Poland. The results of this study provide a new insight into Liparis loeselii ecology. The analysed populations inhabited some habitat types: extremely poor fen, transitional mire, rich fen, calcareous fen, spring-fed fen. The content of nutrients was similar in all the habitats. A CCA analysis revealed that the total carbon content, pH, and redox potential of the substrate determine differences between the habitats analysed. Juvenile individuals represented a maximum of 12% of the analysed populations and were the least abundant group of these plants. The flowering was primarily influenced by hydrological conditions. Based on the long-term observations reported in this article, it can be assumed that the species stands a chance of surviving at the localities analysed, provided that the habitat conditions do not change dramatically.


2016 ◽  
Vol 30 (19) ◽  
pp. 3390-3407 ◽  
Author(s):  
Prasanna Venkatesh Sampath ◽  
Hua-Sheng Liao ◽  
Zachary Kristopher Curtis ◽  
Matthew E. Herbert ◽  
Patrick J. Doran ◽  
...  

ZooKeys ◽  
2018 ◽  
Vol 802 ◽  
pp. 67-108 ◽  
Author(s):  
Maija Štokmane ◽  
Inese Cera

Calcareous fens are one of the most species-rich habitats of the temperate zone of the Northern Hemisphere. In spite of this species richness, however, calcareous fens are still rather poorly investigated. Consequently, the data of the fen-associated spider fauna are also largely lacking. The aim of the research was to study the spider fauna of the calcareous fens of Latvia and to draw conclusions about what kind of spider species and ecological groups typically inhabit calcareous fen habitats. Spiders were sampled in the summer months of 2010, 2011, and 2012 at nine different calcareous fens of the coastal lowland of Latvia. The spider collection was performed by pitfall traps and a sweep net. The examined material comprised 6631 adult spider individuals representing 21 families and 149 species. The main spider ecological groups that dominated in the studied calcareous fens were hygrophilous and photophilous species which largely reflect the main properties of our studied habitats, all of which were wet, open mire habitats. Nevertheless, the fen arachnofauna consisted also of spider groups which are less typical for moist, sun-exposed, and alkaline environments, like xerophilous, sciophilous, and sphagnophilous species, respectively. Finally, several spider species collected in this study have not been previously reported for the spider fauna of Latvia, and many more might still be undiscovered in these unique and poorly investigated habitats. Therefore, it is suggested that calcareous fens deserve special attention and they should definitely be investigated further.


2020 ◽  
Vol 49 (3) ◽  
pp. 723-734
Author(s):  
David Bart ◽  
Eric Booth ◽  
Steven P. Loheide ◽  
Thomas Bernthal

2011 ◽  
Vol 98 (10) ◽  
pp. e290-e292 ◽  
Author(s):  
Yuppayao Kophimai ◽  
Carolina Cornejo ◽  
Markus Peintinger ◽  
Ariel Bergamini ◽  
Christoph Scheidegger

Oikos ◽  
1987 ◽  
Vol 50 (2) ◽  
pp. 183 ◽  
Author(s):  
Matthias W. Diemer ◽  
Jörg Pfadenhauer ◽  
Jorg Pfadenhauer
Keyword(s):  

2008 ◽  
Vol 5 (3) ◽  
pp. 2049-2073
Author(s):  
S. Fiedler ◽  
B. S. Höll ◽  
A. Freibauer ◽  
K. Stahr ◽  
M. Drösler ◽  
...  

Abstract. Numerous studies have dealt with carbon (C) concentrations in Histosols, but there are no studies quantifying the relative importance of all individual C components in pore waters. For this study, measurements were made of all the carbon components (i.e., particulate organic carbon, POC; dissolved organic carbon, DOC; dissolved inorganic carbon, DIC; dissolved methane, CH4) in the soil pore water of a calcareous fen under three different water management regimes (re-wetted, deeply and moderately drained). Pore water was collected weekly or biweekly (April 2004 to April 2006) at depths between 10 and 150 cm. The main results obtained were: (1) DIC (94–280 mg C l−1) was the main C-component. (2) POC and DOC concentrations in the pore water (14–125 mg C l−1 vs. 41–95 mg C l−1) were pari passu. (3) Dissolved CH4 was the smallest C component (0.005–0.9 mg C l−1). Interestingly, about 30% of the POM particles were colonized by microbes indicating that they are active in the internal C transfer in the soil profile ("C-Shuttles"). Consequently, it was concluded that POC is at least as important as DOC for internal soil C turnover. There is no reason to assume significant biochemical differences between POC and DOC as they only differ in size. Therefore, both POC and DOC fractions are essential components of C budgets of peatlands. Furthermore dissolved CO2 in all forms of DIC apparently is an important part of peatland C-balances.


2017 ◽  
Author(s):  
Hannah Francis ◽  
◽  
Josie L. Little ◽  
Casey L. Hecox ◽  
Amy L. Rhodes
Keyword(s):  

Sign in / Sign up

Export Citation Format

Share Document