Response of Landscapes of the Sikhote-Alin Western Slopes to the Middle–Late Holocene Climatic Changes View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2017-12

AUTHORS

N. G. Razzhigaeva, L. A. Ganzey, A. M. Panichev, T. A. Grebennikova, L. M. Mokhova, T. A. Kopoteva, E. P. Kudryavtseva, Kh. A. Arslanov, F. E. Maksimov, A. A. Starikova, S. V. Zakusin

ABSTRACT

The response of landscape biotic components of the western slope of the Sikhote-Alin Mountains (Bikin River middle flow) to the Middle–Late Holocene climate changes is discussed. The paleoreconstruction object was the Krasny Yar mari, which developed under the control of multidirectional short-term climatic changes. The last millennium was marked by particularly rapid and frequent changes in the local landscapes. The closely spaced orographic barrier strongly affected the development of biotic components and changes in the swamp hydrological regime. The moisture dynamics within the river catchment considerably controlled the development and change of the peat-forming plants. Several stages of the mari development were reconstructed; each began from the accumulation of eutrophic peat. It was followed by the transitional eutrophic–mesotrophic stage, with a higher role of atmospheric supply. The larch forests appeared in this part of the valley within the Atlantic–Subboreal cooling period. Korean pine developed in the forest vegetation in the low mountain relief at the beginning of the Subboreal and became one of the leading trees ~2.6–2.3 ka BP. The lower role of the Korean pine and birch forest expansion in the first half of the Subatlantic could be related to the fires. The broadleaf–Korean pine forests became widespread in the Medieval Warm Period. Local swamp landscapes changed dramatically in the Little Ice Age, while the slope vegetation was not subject to any major changes. The landscapes were also affected by the fires, which became more frequent. The derivative communities with birch appeared on the mari. Moreover, this part of the valley was occasionally subject to heavy flooding. More... »

PAGES

679-698

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0001433817070076

DOI

http://dx.doi.org/10.1134/s0001433817070076

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1101303077


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