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5000 ans de dégradation de l'environnement au Lacydon de Marseille
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Zeitschriftentitel: | Méditerranée |
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Personen und Körperschaften: | , |
In: | Méditerranée, 82, 1995, 3, S. 53-62 |
Format: | E-Article |
Sprache: | Französisch |
veröffentlicht: |
PERSEE Program
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Schlagwörter: |
author_facet |
Morhange, Christophe Weydert, Nicolas Morhange, Christophe Weydert, Nicolas |
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author |
Morhange, Christophe Weydert, Nicolas |
spellingShingle |
Morhange, Christophe Weydert, Nicolas Méditerranée 5000 ans de dégradation de l'environnement au Lacydon de Marseille Earth and Planetary Sciences (miscellaneous) Urban Studies Geography, Planning and Development |
author_sort |
morhange, christophe |
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Morhange, Christophe Weydert, Nicolas 0025-8296 PERSEE Program Earth and Planetary Sciences (miscellaneous) Urban Studies Geography, Planning and Development http://dx.doi.org/10.3406/medit.1995.2901 <jats:p>The North shore sediments of the antic harbour of Marseilles reflects a complex history. As early as the Neolithic period, a noticable scouring of soils is identified and related to an extension of anthropisation. The first environmental crisis occured around 3860 ± 130 B.P. (2020 (1865) 1681 cal. B.C.). The silting of the maërl bio-accumulation and the oysters anthropic midden will stop the maërl growth. It is a biological crisis linked with human coastal settlements. No morphological crisis is detected on the hinterland's hills. When Greeks colonized and founded Marseilles around 600 B.C., marine biocenosis of the north shore of the antic harbour were strongly degraded. The successive urbanization of Marseilles' hills will lead to a major detritic crisis. The impact of anthropization is therefore determining after 600 B.C., not only on the shores but also on the hinterland. In comparison, the East shore of the harbour reveals a detritic crisis between 600-400 B.C. and a sedimentary pause during Roman times. These events occured more gradually because of both the presence of coastal swamps and the peri-urban location.</jats:p> 5000 ans de dégradation de l'environnement au Lacydon de Marseille Méditerranée |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au Lacydon de Marseille |
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5000 ans de dégradation de l'environnement au lacydon de marseille |
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Earth and Planetary Sciences (miscellaneous) Urban Studies Geography, Planning and Development |
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http://dx.doi.org/10.3406/medit.1995.2901 |
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1995 |
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<jats:p>The North shore sediments of the antic harbour of Marseilles reflects a complex history. As early as the Neolithic period, a noticable scouring of soils is identified and related to an extension of anthropisation. The first environmental crisis occured around 3860 ± 130 B.P. (2020 (1865) 1681 cal. B.C.). The silting of the maërl bio-accumulation and the oysters anthropic midden will stop the maërl growth. It is a biological crisis linked with human coastal settlements. No morphological crisis is detected on the hinterland's hills. When Greeks colonized and founded Marseilles around 600 B.C., marine biocenosis of the north shore of the antic harbour were strongly degraded. The successive urbanization of Marseilles' hills will lead to a major detritic crisis. The impact of anthropization is therefore determining after 600 B.C., not only on the shores but also on the hinterland. In comparison, the East shore of the harbour reveals a detritic crisis between 600-400 B.C. and a sedimentary pause during Roman times. These events occured more gradually because of both the presence of coastal swamps and the peri-urban location.</jats:p> |
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description | <jats:p>The North shore sediments of the antic harbour of Marseilles reflects a complex history. As early as the Neolithic period, a noticable scouring of soils is identified and related to an extension of anthropisation. The first environmental crisis occured around 3860 ± 130 B.P. (2020 (1865) 1681 cal. B.C.). The silting of the maërl bio-accumulation and the oysters anthropic midden will stop the maërl growth. It is a biological crisis linked with human coastal settlements. No morphological crisis is detected on the hinterland's hills. When Greeks colonized and founded Marseilles around 600 B.C., marine biocenosis of the north shore of the antic harbour were strongly degraded. The successive urbanization of Marseilles' hills will lead to a major detritic crisis. The impact of anthropization is therefore determining after 600 B.C., not only on the shores but also on the hinterland. In comparison, the East shore of the harbour reveals a detritic crisis between 600-400 B.C. and a sedimentary pause during Roman times. These events occured more gradually because of both the presence of coastal swamps and the peri-urban location.</jats:p> |
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spelling | Morhange, Christophe Weydert, Nicolas 0025-8296 PERSEE Program Earth and Planetary Sciences (miscellaneous) Urban Studies Geography, Planning and Development http://dx.doi.org/10.3406/medit.1995.2901 <jats:p>The North shore sediments of the antic harbour of Marseilles reflects a complex history. As early as the Neolithic period, a noticable scouring of soils is identified and related to an extension of anthropisation. The first environmental crisis occured around 3860 ± 130 B.P. (2020 (1865) 1681 cal. B.C.). The silting of the maërl bio-accumulation and the oysters anthropic midden will stop the maërl growth. It is a biological crisis linked with human coastal settlements. No morphological crisis is detected on the hinterland's hills. When Greeks colonized and founded Marseilles around 600 B.C., marine biocenosis of the north shore of the antic harbour were strongly degraded. The successive urbanization of Marseilles' hills will lead to a major detritic crisis. The impact of anthropization is therefore determining after 600 B.C., not only on the shores but also on the hinterland. In comparison, the East shore of the harbour reveals a detritic crisis between 600-400 B.C. and a sedimentary pause during Roman times. These events occured more gradually because of both the presence of coastal swamps and the peri-urban location.</jats:p> 5000 ans de dégradation de l'environnement au Lacydon de Marseille Méditerranée |
spellingShingle | Morhange, Christophe, Weydert, Nicolas, Méditerranée, 5000 ans de dégradation de l'environnement au Lacydon de Marseille, Earth and Planetary Sciences (miscellaneous), Urban Studies, Geography, Planning and Development |
title | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
title_full | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
title_fullStr | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
title_full_unstemmed | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
title_short | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
title_sort | 5000 ans de dégradation de l'environnement au lacydon de marseille |
title_unstemmed | 5000 ans de dégradation de l'environnement au Lacydon de Marseille |
topic | Earth and Planetary Sciences (miscellaneous), Urban Studies, Geography, Planning and Development |
url | http://dx.doi.org/10.3406/medit.1995.2901 |