Collembola of forest tundra ecosystems of the Sula (Malozemelskaya tundra) and Bolshaya Rogovaya (Bolshezemelskaya tundra) rivers

Registros de Dados

Os dados deste recurso de evento de amostragem foram publicados como um Darwin Core Archive (DwC-A), que é o formato padronizado para compartilhamento de dados de biodiversidade como um conjunto de uma ou mais tabelas de dados. A tabela de dados do núcleo contém 124 registros.

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Versões

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Como citar

Pesquisadores deveriam citar esta obra da seguinte maneira:

Lapteva E.M., Deneva S.V., Degteva S.V. 2020. Floodplain soils of river valleys as an object of special protection in the Komi Rrepublic’s system of protected areas // Transactions of Karelian Research Centre of the Russian Academy of Sciences. No.8. P. 46‒64. doi: 10.17076/bg1155 [in Russian].

Direitos

Pesquisadores devem respeitar a seguinte declaração de direitos:

O editor e o detentor dos direitos deste trabalho é Institute of Biology of Komi Scientific Centre of the Ural Branch of the Russian Academy of Sciences. This work is licensed under a Creative Commons Attribution Non Commercial (CC-BY-NC 4.0) License.

GBIF Registration

Este recurso foi registrado no GBIF e atribuído ao seguinte GBIF UUID: 64554fb1-f4ae-41f3-a63f-98485c540ab7.  Institute of Biology of Komi Scientific Centre of the Ural Branch of the Russian Academy of Sciences publica este recurso, e está registrado no GBIF como um publicador de dados aprovado por Participant Node Managers Committee.

Palavras-chave

Samplingevent; forest tundra ecosystems; springtails

Contatos

Cobertura Geográfica

The Sula River is one of the Timan tributaries of the lower reaches of the Pechora river. The Timan Ridge itself stretches from the Czech Bay of the Arctic Ocean to the head of the Vychegda river in the foothills of the Urals and is a flattened ridge 950 km long with separate low ridges, located in the northeast of the East European Plain. The Bolshaya Rogovaya River originates in the northeastern tip of the Chernyshev Ridge. Its valley is a flat plain with a large number of lakes and absolute elevations of 80–100 m. The depressions and ravines of the runoff are often covered with thickets of tree-like willow and juniper. Shrub moss-lichen tundras develop on drained massivs. Separate massifs of spruce-birch light forests are confined mainly to river valleys. In 2019, the "Bolshaya Rogovaya Reserve" was created here, which performs the functions of preserving floodplain soils (Lapteva et al., 2020).

Cobertura Taxonômica

Nenhuma descrição disponível

Cobertura Temporal

Métodos de Amostragem

On the territory of the Sula river basin six plots were studied. They are floodplain and mixed grass meadows, birch spruce forest, dwarf shrub lichen, dwarf shrub grass and dwarf birch tundra. On the territory of the Bolshaya Rogovaya river 11 sites were studied. They are: association with Equisétum, herb-grass, grass and tall-grass meadows, Juniper community, willows, different types of birch and spruce forests, which are situated in the floodplain of the river. The other five sites are located in the plain and presented by the next plant communities: sedge association, palsa mires, birch forest, dwarf shrub lichen and dwarf shrub moss lichen tundra.

Descrição dos passos do método:

1. On the territory of the Sula river 10 soil samples of 100 cm2 were taken at each plot at a depth of the organogenic horizon of 4–10 cm. On the territory of the Bolshaya Rogovaya river 3-15 soil samples of 25 cm2 were taken at each site.

Metadados Adicionais