scholarly journals Fauna and ecology of Hymenoptera background species of terrestrial ecosystems in the Yenisei Siberia tundra and forest-tundra

2020 ◽  
Vol 9 (3) ◽  
pp. 21-27
Author(s):  
Aleksander A. Baranov ◽  
Emilia V. Stambrovskaya ◽  
Svetlana N. Gorodilova ◽  
Ksenia K. Bannikova ◽  
Olga N. Melnik

This paper presents materials on the ecology and faunistic composition of four species of Hymenoptera: Urocerus gigas L., 1758; Vespula vulgaris L., 1758; Bombus polaris Curtis, 1835; Bombus hyperboreus Schonherr, 1809. Their number was calculated for 20172019, data on population density, seasonal activity and forage plants of Hymenoptera adults in the tundra and forest-tundra of Yenisei Siberia are presented. As a result of calculating in both natural conditions, numerous species are true wasps and bumblebees and the large horntail is a rare species and was recorded only in the forest-tundra. When studying the food base of the studied species, it was noted that Vespula vulgaris was most often found on the forest bellap Anthriscus sylvestris L., in thickets of willow shrubs, Salix polaris Wahlenb. Adult insects Urocerus gigas were found mainly on Siberian larch Larix sibirica L. and alder forest Alnus fruticosa Rupr. Individuals of Bombus polaris and Bombus hyperboreus were recorded on horned dandelion Taraxacum ceratophorum L., narrow-leaved fireweed Chamerion angustifolium L., common tansy Tanacetum vulgare L.

Soil Systems ◽  
2020 ◽  
Vol 4 (1) ◽  
pp. 14 ◽  
Author(s):  
Gerald Jurasinski ◽  
Sate Ahmad ◽  
Alba Anadon-Rosell ◽  
Jacqueline Berendt ◽  
Florian Beyer ◽  
...  

Of all terrestrial ecosystems, peatlands store carbon most effectively in long-term scales of millennia. However, many peatlands have been drained for peat extraction or agricultural use. This converts peatlands from sinks to sources of carbon, causing approx. 5% of the anthropogenic greenhouse effect and additional negative effects on other ecosystem services. Rewetting peatlands can mitigate climate change and may be combined with management in the form of paludiculture. Rewetted peatlands, however, do not equal their pristine ancestors and their ecological functioning is not understood. This holds true especially for groundwater-fed fens. Their functioning results from manifold interactions and can only be understood following an integrative approach of many relevant fields of science, which we merge in the interdisciplinary project WETSCAPES. Here, we address interactions among water transport and chemistry, primary production, peat formation, matter transformation and transport, microbial community, and greenhouse gas exchange using state of the art methods. We record data on six study sites spread across three common fen types (Alder forest, percolation fen, and coastal fen), each in drained and rewetted states. First results revealed that indicators reflecting more long-term effects like vegetation and soil chemistry showed a stronger differentiation between drained and rewetted states than variables with a more immediate reaction to environmental change, like greenhouse gas (GHG) emissions. Variations in microbial community composition explained differences in soil chemical data as well as vegetation composition and GHG exchange. We show the importance of developing an integrative understanding of managed fen peatlands and their ecosystem functioning.


Author(s):  
Gerald Jurasinski ◽  
Sate Ahmad ◽  
Alba Anadon-Rosell ◽  
Jacqueline Berendt ◽  
Florian Beyer ◽  
...  

Of all terrestrial ecosystems, peatlands store carbon most effectively in long-term scales of millennia. However, many peatlands have been drained for peat extraction or agricultural use. This converts peatlands from sinks to sources of carbon, causing approx. 5% of the anthropogenic greenhouse effect and additional negative effects on other ecosystem services. Rewetting peatlands can mitigate climate change and may be combined with management in the form of paludiculture. Rewetted peatlands, however, do not equal their pristine ancestors and their ecological functioning is not understood. This holds especially for groundwater-fed fens. Their functioning results from manifold interactions and can only be understood following an integrative approach of many relevant fields of science, which we merge in the interdisciplinary project WETSCAPES. Here, we address interactions among water transport and chemistry, primary production, peat formation, matter transformation and transport, microbial community and greenhouse gas exchange using state of the art methods. We record data on six study sites spreading across three common fen types (Alder forest, percolation fen, and coastal fen) each in drained and rewetted state. First results showed that indicators reflecting more long-term effects like vegetation and soil chemistry showed a stronger differentiation between drained and rewetted state than variables with more immediate reaction to environmental change, like greenhouse gas (GHG) emissions. Variations in microbial community composition explained differences in soil chemical data as well as vegetation composition and GHG exchange. We show the importance of developing an integrative understanding of managed fen peatlands and their ecosystem functioning.


2019 ◽  
pp. 309-316
Author(s):  
Ольга (Ol'ga) Владимировна (Vladimirovna) Калугина (Kalugina) ◽  
Татьяна (Tat'yana) Алексеевна (Alekseevna) Михайлова (Mikhailova) ◽  
Ольга (Ol'ga) Владимировна (Vladimirovna) Шергина (Shergina)

Specific features of fluoride accumulation by two species of herbaceous plants – Chamerion angustifolium (L.) Holub and Tanacetum vulgare L., were found at different distances from the aluminum smelter located in the Baikal region. The highest fluorine content was recorded at the distance of 3 km from the smelter: 433 mg / kg of dry weight in C. angustifolium, 306 mg / kg in T. vulgare. According to the level of accumulation of fluorine, the organs of C. angustifolium were arranged in the following order (as the concentration decreases): leaves> roots> stems ≥ flowers, for T. vulgare the another sequence was typical: roots> leaves> flowers ≥ stems. Calculation of the root barrier coefficient for different organs of C. angustifolium and T. vulgare indicates the existence of barrier mechanisms that prevent the entry of fluorine from the soil into the aerial part of plants. A feature of the accumulation of fluoride in the leaves of C. angustifolium is its active foliar absorption and barrier-free intake from the soil. It has been established that the rate of fluoride accumulation by the reproductive organs of both species is much lower than by the assimilation organs. The data obtained make it possible to recommend using C. angustifolium for monitoring air fluorine pollution, and T. vulgare – for soil fluorine pollution.


2020 ◽  
Vol 48 (3) ◽  
pp. 80-89
Author(s):  
V. S. Myglan ◽  
G. T. Omurova ◽  
V. V. Barinov ◽  
O. V. Kardash

Archaeological studies in the forest-tundra zone of Western Siberia are highly relevant to studying the material culture, social structure, and ethnic history. The presence of permafrost ensures the unique preservation of organics in cultural layers, including timber, which makes it possible to conduct dendrochronological studies (calendar dating of samples, determination of species composition, typological analysis, and the source of the timber origin). In 2011–2012, during the excavations at Fort Nadym, 347 samples of wood were selected for the assessment of the age of wooden structures. The results showed that most samples belonged to three species of trees: Siberian larch (Larix sibirica Ledeb.), Siberian spruce (Picea obovata Ledeb.), and Siberian pine (Pinus sibirica Du Tour). The typological analysis revealed that walls were mostly built from spruce, pine logs, and half-logs, whereas the floors were made from larch and pine. To assess the origin of wood, a new methodological approach was proposed. As a result, it was demonstrated that the main building material was driftwood. This has allowed us to make more accurate interpretations and to specify the years of construction. The analysis indicates three periods of construction / reconstruction: the 1450s–1460s, 1470s–1480s, and 1520s–1570s. The new approach can be applied to other wooden monuments located on the banks of major water arteries of the Siberian forest-tundra zone.


Author(s):  
Gerald Jurasinski ◽  
Sate Ahmad ◽  
Alba Anadon-Rosell ◽  
Jacqueline Berendt ◽  
Florian Beyer ◽  
...  

Of all terrestrial ecosystems, peatlands store carbon most effectively. However, many peatlands have been drained for peat extraction or agricultural use. This converts peatlands from sinks to sources of carbon, causing approx. 5% of the anthropogenic greenhouse effect and additional negative effects on other ecosystem services. Rewetting peatlands can mitigate the climate crisis and may be combined with management in the form of paludiculture. Rewetted peatlands, however, do not equal their pristine ancestors and their ecological functioning is not understood. This holds especially for fens. Their functioning results from complex interactions and can only be understood following an integrative approach of many relevant fields of science, which we develop in the interdisciplinary project WETSCAPES. Here, we introduce our approach in which we are addressing interactions among water transport and chemistry, primary production, peat formation, matter transformation and transport, microorganisms and greenhouse gas exchange using state of the art methods in the relevant research fields. We record data on six study sites spreading across three important fen types (Alder forest, percolation fen, and coastal fen) each in drained and rewetted state. Using exemplary results, we show the importance of developing an integrative understanding of managed fen peatlands and their ecosystem functioning.


1999 ◽  
Vol 13 (3) ◽  
pp. 751-760 ◽  
Author(s):  
Nina Buchmann

2017 ◽  
Vol 262 (02) ◽  
pp. 2-76
Author(s):  
L Kosmodemyanskiy ◽  
D Popov ◽  
S Popova ◽  
A Fadiev

Planta Medica ◽  
2007 ◽  
Vol 73 (09) ◽  
Author(s):  
G Horváth ◽  
E Turcsi ◽  
P Molnár ◽  
LG Szabó ◽  
J Deli

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