Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Vegetation of sandy outcrops in Pechora tundra

View through CrossRef
The paper deals with the syntaxonomy of vegetation on the sandy outcrops in the Pechora (Malozemelskaya and Bolshezemelskaya) tundra. The vegetation was classified using the Brown-Blanke approach. Communities were referred to 3 associations: Arctostaphylo alpini—Empetretum hermaphroditi (Zinserling 1935) Koroleva 1994, Elymo—Festucetum arenariae (Regel 1923) Nordhagen 1955 and Rumici graminifoliae—Festucetum sabulosae ass. nov. Five new variants were suggested within the first association and 2 subassociations and 4 variants within the last one. Syntaxon description and phytocoenological tables are presented. The vegetation on each sandy outcrops represents a complex of communities fragmentary located on the scars area. Subass. inops of ass. Rumici graminifoliae—Festucetum sabulosae is more common in the Ortina river basin and occurs at the bottom of blowing hollows. Syntaxa of ass. Elymo—Festucetum arenariae and var. Festuca rubra of ass. Rumici graminifoliae—Festucetum sabulosae are situated at the mobile sands in the central part, while var. Arctous alpina of ass. Rumici graminifoliae—Festucetum sabulosae occurs on a periphery of out­crops where substratum is stable. The variants inops and typicum of ass. Arctostaphylo alpini—Empetretum hermaphroditi occuring in the Sedujyakha river basin occur mostly in the centre of sandy outcrops, and the other ones can be met on their periphery. Ecological conditions determine poor diversity of syntaxa of the association level. Geographical position (the Sedujyakha river basin belongs to the northern hypoarctic tundras, the Ortina river basin — to the southern hypoarctic ones), geomorphology (in the first site — tops of hills and ridges, in the second one — watershed areas) and area of sandy outcrops (200—3000 m2 for the first and 61000—418000 m2 for the second site respectively) are the reasons for the less diverse communities found in each study site. A great number of variants is conditioned by succession stages of vegetation and instability of the substrates.
Komarov Botanical Institute of the Russian Academy of Sciences
Title: Vegetation of sandy outcrops in Pechora tundra
Description:
The paper deals with the syntaxonomy of vegetation on the sandy outcrops in the Pechora (Malozemelskaya and Bolshezemelskaya) tundra.
The vegetation was classified using the Brown-Blanke approach.
Communities were referred to 3 associations: Arctostaphylo alpini—Empetretum hermaphroditi (Zinserling 1935) Koroleva 1994, Elymo—Festucetum arenariae (Regel 1923) Nordhagen 1955 and Rumici graminifoliae—Festucetum sabulosae ass.
nov.
Five new variants were suggested within the first association and 2 subassociations and 4 variants within the last one.
Syntaxon description and phytocoenological tables are presented.
The vegetation on each sandy outcrops represents a complex of communities fragmentary located on the scars area.
Subass.
inops of ass.
Rumici graminifoliae—Festucetum sabulosae is more common in the Ortina river basin and occurs at the bottom of blowing hollows.
Syntaxa of ass.
Elymo—Festucetum arenariae and var.
Festuca rubra of ass.
Rumici graminifoliae—Festucetum sabulosae are situated at the mobile sands in the central part, while var.
Arctous alpina of ass.
Rumici graminifoliae—Festucetum sabulosae occurs on a periphery of out­crops where substratum is stable.
The variants inops and typicum of ass.
Arctostaphylo alpini—Empetretum hermaphroditi occuring in the Sedujyakha river basin occur mostly in the centre of sandy outcrops, and the other ones can be met on their periphery.
Ecological conditions determine poor diversity of syntaxa of the association level.
Geographical position (the Sedujyakha river basin belongs to the northern hypoarctic tundras, the Ortina river basin — to the southern hypoarctic ones), geomorphology (in the first site — tops of hills and ridges, in the second one — watershed areas) and area of sandy outcrops (200—3000 m2 for the first and 61000—418000 m2 for the second site respectively) are the reasons for the less diverse communities found in each study site.
A great number of variants is conditioned by succession stages of vegetation and instability of the substrates.

Related Results

Late Quaternary History of Tundra Vegetation in Northwestern Alaska
Late Quaternary History of Tundra Vegetation in Northwestern Alaska
AbstractPollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra type...
Sub-bottom Permafrost and Shallow Gas in Pechora Sea
Sub-bottom Permafrost and Shallow Gas in Pechora Sea
Abstract Joint research Russian-Finnish expeditions have been carried out to eastern Pechora Sea, in order to investigate the setting of Pleistocene-Holocene sedi...
Impact of vegetation control measures on the bedform of braided gravel-bed river
Impact of vegetation control measures on the bedform of braided gravel-bed river
<p>Braiding is among the most dynamic landscape on Earth. It provides diverse habitats for freshwater creatures. Unfortunately, the number of braided rivers is reduci...
Post-fire vegetation succession in the Siberian subarctic tundra over 45 years
Post-fire vegetation succession in the Siberian subarctic tundra over 45 years
Abstract Wildfires are relatively rare in subarctic tundra ecosystems, but they can strongly change ecosystem properties. Short-term fire effects on subarctic tundr...
Long‐term recovery patterns of arctic tundra after winter seismic exploration
Long‐term recovery patterns of arctic tundra after winter seismic exploration
In response to the increasing global demand for energy, oil exploration and development are expanding into frontier areas of the Arctic, where slow‐growing tundra vegetation and th...
Incorporating Vegetation Type Transformation with NDVI Time-Series to Study the Vegetation Dynamics in Xinjiang
Incorporating Vegetation Type Transformation with NDVI Time-Series to Study the Vegetation Dynamics in Xinjiang
Time-series normalized difference vegetation index (NDVI) is commonly used to conduct vegetation dynamics, which is an important research topic. However, few studies have focused o...
Vegetation mapping at Horseshoe Bend National Military Park: Photointerpretation key and final vegetation map
Vegetation mapping at Horseshoe Bend National Military Park: Photointerpretation key and final vegetation map
The University of Georgia Department of Geography’s Center for Geospatial Research (CGR), with the support of the National Park Service (NPS) Vegetation Mapping Inventory (VMI) Pro...
The morphology of experimentally produced charcoal distinguishes fuel types in the Arctic tundra
The morphology of experimentally produced charcoal distinguishes fuel types in the Arctic tundra
Wildfires in the Arctic tundra have become increasingly frequent in recent years and have important implications for tundra ecosystems and for the global carbon cycle. Lake sedimen...

Back to Top