Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV

Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Numata, Makoto [verfasserIn]

Format:	Artikel
Sprache:	Englisch

Erschienen:	1969

Schlagwörter:	Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage

Anmerkung:	© Dr W. Junk N. V. 1969

Übergeordnetes Werk:	Enthalten in: Vegetatio - Kluwer Academic Publishers, 1948, 19(1969), 1-6 vom: Jan., Seite 96-127
Übergeordnetes Werk:	volume:19 ; year:1969 ; number:1-6 ; month:01 ; pages:96-127

Links:	Volltext

DOI / URN:	10.1007/BF00259006

Katalog-ID:	OLC208423364X

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520			\|a Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself.
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allfields	10.1007/BF00259006 doi (DE-627)OLC208423364X (DE-He213)BF00259006-p DE-627 ger DE-627 rakwb eng 580 VZ 12 ssgn BIODIV DE-30 fid Numata, Makoto verfasserin aut Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Dr W. Junk N. V. 1969 Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage Enthalten in Vegetatio Kluwer Academic Publishers, 1948 19(1969), 1-6 vom: Jan., Seite 96-127 (DE-627)129466557 (DE-600)201543-2 (DE-576)014832917 0042-3106 nnns volume:19 year:1969 number:1-6 month:01 pages:96-127 https://doi.org/10.1007/BF00259006 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_211 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4155 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4323 GBV_ILN_4325 AR 19 1969 1-6 01 96-127
spelling	10.1007/BF00259006 doi (DE-627)OLC208423364X (DE-He213)BF00259006-p DE-627 ger DE-627 rakwb eng 580 VZ 12 ssgn BIODIV DE-30 fid Numata, Makoto verfasserin aut Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Dr W. Junk N. V. 1969 Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage Enthalten in Vegetatio Kluwer Academic Publishers, 1948 19(1969), 1-6 vom: Jan., Seite 96-127 (DE-627)129466557 (DE-600)201543-2 (DE-576)014832917 0042-3106 nnns volume:19 year:1969 number:1-6 month:01 pages:96-127 https://doi.org/10.1007/BF00259006 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_211 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4155 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4323 GBV_ILN_4325 AR 19 1969 1-6 01 96-127
allfields_unstemmed	10.1007/BF00259006 doi (DE-627)OLC208423364X (DE-He213)BF00259006-p DE-627 ger DE-627 rakwb eng 580 VZ 12 ssgn BIODIV DE-30 fid Numata, Makoto verfasserin aut Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Dr W. Junk N. V. 1969 Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage Enthalten in Vegetatio Kluwer Academic Publishers, 1948 19(1969), 1-6 vom: Jan., Seite 96-127 (DE-627)129466557 (DE-600)201543-2 (DE-576)014832917 0042-3106 nnns volume:19 year:1969 number:1-6 month:01 pages:96-127 https://doi.org/10.1007/BF00259006 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_211 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4155 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4323 GBV_ILN_4325 AR 19 1969 1-6 01 96-127
allfieldsGer	10.1007/BF00259006 doi (DE-627)OLC208423364X (DE-He213)BF00259006-p DE-627 ger DE-627 rakwb eng 580 VZ 12 ssgn BIODIV DE-30 fid Numata, Makoto verfasserin aut Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV 1969 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Dr W. Junk N. V. 1969 Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage Enthalten in Vegetatio Kluwer Academic Publishers, 1948 19(1969), 1-6 vom: Jan., Seite 96-127 (DE-627)129466557 (DE-600)201543-2 (DE-576)014832917 0042-3106 nnns volume:19 year:1969 number:1-6 month:01 pages:96-127 https://doi.org/10.1007/BF00259006 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-UMW SSG-OLC-TEC SSG-OLC-FOR SSG-OPC-FOR GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_211 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4035 GBV_ILN_4082 GBV_ILN_4155 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4311 GBV_ILN_4323 GBV_ILN_4325 AR 19 1969 1-6 01 96-127
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language	English
source	Enthalten in Vegetatio 19(1969), 1-6 vom: Jan., Seite 96-127 volume:19 year:1969 number:1-6 month:01 pages:96-127
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author	Numata, Makoto
spellingShingle	Numata, Makoto ddc 580 ssgn 12 fid BIODIV misc Alpine Grassland misc Grassland Vegetation misc Dynamic Ecology misc Grassland Type misc Seral Stage Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV
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topic_title	580 VZ 12 ssgn BIODIV DE-30 fid Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV Alpine Grassland Grassland Vegetation Dynamic Ecology Grassland Type Seral Stage
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title	Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV
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title_full	Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV
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title_sort	progressive and retrogressive gradient of grassland vegetation measured by degree of succession—ecological judgement of grassland condition and trend iv
title_auth	Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV
abstract	Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. © Dr W. Junk N. V. 1969
abstractGer	Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. © Dr W. Junk N. V. 1969
abstract_unstemmed	Summary The types of grassland vegetation expressed by the dominants were surveyed from north to south in Japan, and their successional and climatic relationships were given from the viewpoint of quantitative and dynamic ecology (Table I, Figs. 1–3). There are many grassland types in Japan, but only major types were dealt with, compared by some characteristics (location, use, dominant, ground cover of vegetation (v), number of constituent species (n), degree of succession (DS), summed dominance ratio (SDR), and relative SDR (SDR′) and showing each example of the floristic composition (Tables II–XIII). The grassland vegetation in Japan is not the climatic climax but seral stages, except alpine grasslands over the tree line of high mountains. There are two cases in grassland succession, orthosere and plagiosere. “Orthosere” is the ordinary subsere in the abandoned field lacking biotic suppressions, however “plagiosere” is the gradient under biotic pressures such as grazing, mowing, burning, etc. The latter is mostly dealt with in this paper. The ordination of various grassland types in the DS-frequency relationships is given in Fig. 4. This is not a real course of the grassland succession, but ecological gradient of grassland types. Such an ordination of grassland vegetation in a given area may show the seral status itself. © Dr W. Junk N. V. 1969
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title_short	Progressive and retrogressive gradient of grassland vegetation measured by degree of succession—Ecological judgement of grassland condition and trend IV
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