Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state
Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been tra...
Ausführliche Beschreibung
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De Gruyter Open ; 2016 |
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11 |
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Walter de Gruyter Online Zeitschriften |
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Übergeordnetes Werk: |
Enthalten in: Hacquetia - Ljubljana : Založba ZRC, 2002, 15(2016), 2 vom: 12. Aug., Seite 37-47 |
Übergeordnetes Werk: |
volume:15 ; year:2016 ; number:2 ; day:12 ; month:08 ; pages:37-47 ; extent:11 |
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DOI / URN: |
10.1515/hacq-2016-0016 |
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NLEJ24801059X |
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10.1515/hacq-2016-0016 doi articles2015-2020.pp (DE-627)NLEJ24801059X DE-627 ger DE-627 rakwb Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state De Gruyter Open 2016 11 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. Walter de Gruyter Online Zeitschriften buried soils ecosystem convergence land use history mountain meadow-steppes semi-natural grasslands subalpine meadows Belonovskaya, Elena oth Gracheva, Raisa oth Shorkunov, Ilya oth Vinogradova, Vera oth Enthalten in Hacquetia Ljubljana : Založba ZRC, 2002 15(2016), 2 vom: 12. Aug., Seite 37-47 (DE-627)NLEJ248237284 (DE-600)2406488-9 1854-9829 nnns volume:15 year:2016 number:2 day:12 month:08 pages:37-47 extent:11 https://doi.org/10.1515/hacq-2016-0016 Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-DGR GBV_NL_ARTICLE AR 15 2016 2 12 8 37-47 11 |
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10.1515/hacq-2016-0016 doi articles2015-2020.pp (DE-627)NLEJ24801059X DE-627 ger DE-627 rakwb Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state De Gruyter Open 2016 11 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. Walter de Gruyter Online Zeitschriften buried soils ecosystem convergence land use history mountain meadow-steppes semi-natural grasslands subalpine meadows Belonovskaya, Elena oth Gracheva, Raisa oth Shorkunov, Ilya oth Vinogradova, Vera oth Enthalten in Hacquetia Ljubljana : Založba ZRC, 2002 15(2016), 2 vom: 12. Aug., Seite 37-47 (DE-627)NLEJ248237284 (DE-600)2406488-9 1854-9829 nnns volume:15 year:2016 number:2 day:12 month:08 pages:37-47 extent:11 https://doi.org/10.1515/hacq-2016-0016 Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-DGR GBV_NL_ARTICLE AR 15 2016 2 12 8 37-47 11 |
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10.1515/hacq-2016-0016 doi articles2015-2020.pp (DE-627)NLEJ24801059X DE-627 ger DE-627 rakwb Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state De Gruyter Open 2016 11 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. Walter de Gruyter Online Zeitschriften buried soils ecosystem convergence land use history mountain meadow-steppes semi-natural grasslands subalpine meadows Belonovskaya, Elena oth Gracheva, Raisa oth Shorkunov, Ilya oth Vinogradova, Vera oth Enthalten in Hacquetia Ljubljana : Založba ZRC, 2002 15(2016), 2 vom: 12. Aug., Seite 37-47 (DE-627)NLEJ248237284 (DE-600)2406488-9 1854-9829 nnns volume:15 year:2016 number:2 day:12 month:08 pages:37-47 extent:11 https://doi.org/10.1515/hacq-2016-0016 Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-DGR GBV_NL_ARTICLE AR 15 2016 2 12 8 37-47 11 |
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10.1515/hacq-2016-0016 doi articles2015-2020.pp (DE-627)NLEJ24801059X DE-627 ger DE-627 rakwb Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state De Gruyter Open 2016 11 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. Walter de Gruyter Online Zeitschriften buried soils ecosystem convergence land use history mountain meadow-steppes semi-natural grasslands subalpine meadows Belonovskaya, Elena oth Gracheva, Raisa oth Shorkunov, Ilya oth Vinogradova, Vera oth Enthalten in Hacquetia Ljubljana : Založba ZRC, 2002 15(2016), 2 vom: 12. Aug., Seite 37-47 (DE-627)NLEJ248237284 (DE-600)2406488-9 1854-9829 nnns volume:15 year:2016 number:2 day:12 month:08 pages:37-47 extent:11 https://doi.org/10.1515/hacq-2016-0016 Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-DGR GBV_NL_ARTICLE AR 15 2016 2 12 8 37-47 11 |
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10.1515/hacq-2016-0016 doi articles2015-2020.pp (DE-627)NLEJ24801059X DE-627 ger DE-627 rakwb Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state De Gruyter Open 2016 11 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. Walter de Gruyter Online Zeitschriften buried soils ecosystem convergence land use history mountain meadow-steppes semi-natural grasslands subalpine meadows Belonovskaya, Elena oth Gracheva, Raisa oth Shorkunov, Ilya oth Vinogradova, Vera oth Enthalten in Hacquetia Ljubljana : Založba ZRC, 2002 15(2016), 2 vom: 12. Aug., Seite 37-47 (DE-627)NLEJ248237284 (DE-600)2406488-9 1854-9829 nnns volume:15 year:2016 number:2 day:12 month:08 pages:37-47 extent:11 https://doi.org/10.1515/hacq-2016-0016 Deutschlandweit zugänglich GBV_USEFLAG_U ZDB-1-DGR GBV_NL_ARTICLE AR 15 2016 2 12 8 37-47 11 |
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Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state |
abstract |
Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. |
abstractGer |
Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. |
abstract_unstemmed |
Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. It is assumed that the present convergence of soil cover and vegetation is a result of long homogenising human impact and relatively short grassland development. |
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10.1515/hacq-2016-0016 |
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2024-07-05T22:19:49.894Z |
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1803779298974236672 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ24801059X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220820035307.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220814s2016 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1515/hacq-2016-0016</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">articles2015-2020.pp</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ24801059X</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Grasslands of intermontane basins of Central Caucasus: land use legacies and present-day state</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="b">De Gruyter Open</subfield><subfield code="c">2016</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">11</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Mountain semi-natural grasslands of intermontane basins of Central Caucasus, North Ossetia-Alania and the history of its land use were studied. It was found that post-forest, meadow-steppe and partially subalpine grasslands in the study area had been used as croplands for centuries and have been transformed into grazing lands about 60 years ago. In the last 20 years, the grasslands have been underused. It was revealed that current spatial distribution of grasslands is different from the classic scheme of natural climate-induced vegetation distribution. Species composition of meadow steppes is similar in different locations and does not reflect climatic differences of “dry” leeward and “wet” windward slopes of the intermontane basins. Present-day soils reflect parent material differences and erosion degree, but not topography-induced local climate specificity. However, discovered buried soils showed contrasting soil diversity on the southern and northern slopes. 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Aug., Seite 37-47</subfield><subfield code="w">(DE-627)NLEJ248237284</subfield><subfield code="w">(DE-600)2406488-9</subfield><subfield code="x">1854-9829</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:2</subfield><subfield code="g">day:12</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:37-47</subfield><subfield code="g">extent:11</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1515/hacq-2016-0016</subfield><subfield code="z">Deutschlandweit zugänglich</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DGR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">15</subfield><subfield code="j">2016</subfield><subfield code="e">2</subfield><subfield code="b">12</subfield><subfield code="c">8</subfield><subfield code="h">37-47</subfield><subfield code="g">11</subfield></datafield></record></collection>
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