Add to ORKG© 2018, Pleiades Publishing, Ltd. The use of chironomids (Diptera: Chironomidae) as indicators of changes in natural and climatic settings allows one to reconstruct paleoclimatic and paleoenvironmental conditions. Based on the results of lithological and chironomid analyses, the loss on ignition (LOI) values, as well as the results of radiocarbon dating (14C AMS), new data on the paleoclimate in the Karelian Isthmus, in particular the quantitative reconstruction of the mean July temperature (TJuly, °C) in the Late Pleistocene and Holocene and the evolution of the ecosystem of Medvedevskoe Lake have been obtained
A 380 cm long sediment core from Lake Temje (central Yakutia, Eastern Siberia) was studied to infer ...
International audienceWe present a chironomid-based reconstruction of late-Holocene temperature from...
Chironomid remains from the sediment of Lake Vuolep Njakajaure reflect limnological conditions resul...
© 2018, Pleiades Publishing, Ltd. The use of chironomids (Diptera: Chironomidae) as indicators of ch...
The use of chironomids (Diptera: Chironomidae) as indicators of changes in natural and climatic sett...
A radiocarbon-dated sediment sequence from Lake Berkut in the southern part of the Kola Peninsula, n...
We present a new chironomid record from sediments of former Lake ˇSvarcenberk in South Bohemia (412 ...
A 380 cm long sediment core from Lake Temje (central Yakutia, Eastern Siberia) was studied to infer ...
This paper examines the environmental and climatic changes during Late Glacial and Early Holocene, b...
This study presents a reconstruction of the Late Holocene climate in Kamchatka based on chironomid r...
The Holocene evolution of climate in easternmost Fennoscandia and adjoining regions is poorly known,...
The last interglacial-glacial cycle represents an interval in which a broad range of climatic condit...
The reconstruction of the dynamic elements of past environments is extremely important for understan...
Temperature reconstructions for the end of the Pleistocene and the first half of the Holocene based ...
We studied a sediment core from the lake Khatanga-12 (Taimyr Peninsula, Krasnoyarsk region). The cor...
A 380 cm long sediment core from Lake Temje (central Yakutia, Eastern Siberia) was studied to infer ...
International audienceWe present a chironomid-based reconstruction of late-Holocene temperature from...
Chironomid remains from the sediment of Lake Vuolep Njakajaure reflect limnological conditions resul...
© 2018, Pleiades Publishing, Ltd. The use of chironomids (Diptera: Chironomidae) as indicators of ch...
The use of chironomids (Diptera: Chironomidae) as indicators of changes in natural and climatic sett...
A radiocarbon-dated sediment sequence from Lake Berkut in the southern part of the Kola Peninsula, n...
We present a new chironomid record from sediments of former Lake ˇSvarcenberk in South Bohemia (412 ...
A 380 cm long sediment core from Lake Temje (central Yakutia, Eastern Siberia) was studied to infer ...
This paper examines the environmental and climatic changes during Late Glacial and Early Holocene, b...
This study presents a reconstruction of the Late Holocene climate in Kamchatka based on chironomid r...
The Holocene evolution of climate in easternmost Fennoscandia and adjoining regions is poorly known,...
The last interglacial-glacial cycle represents an interval in which a broad range of climatic condit...
The reconstruction of the dynamic elements of past environments is extremely important for understan...
Temperature reconstructions for the end of the Pleistocene and the first half of the Holocene based ...
We studied a sediment core from the lake Khatanga-12 (Taimyr Peninsula, Krasnoyarsk region). The cor...
A 380 cm long sediment core from Lake Temje (central Yakutia, Eastern Siberia) was studied to infer ...
International audienceWe present a chironomid-based reconstruction of late-Holocene temperature from...
Chironomid remains from the sediment of Lake Vuolep Njakajaure reflect limnological conditions resul...