The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps)
Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top:...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gaetani, Maurizio [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1989 |
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| Schlagwörter: |
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| Anmerkung: |
© Institut für Paläontologie, Universität Erlangen 1989 |
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| Übergeordnetes Werk: |
Enthalten in: Facies - Springer-Verlag, 1979, 21(1989), 1 vom: Dez., Seite 41-56 |
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| Übergeordnetes Werk: |
volume:21 ; year:1989 ; number:1 ; month:12 ; pages:41-56 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02536831 |
|---|
| Katalog-ID: |
OLC2075392218 |
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| 245 | 1 | 0 | |a The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) |
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| 520 | |a Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. | ||
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10.1007/BF02536831 doi (DE-627)OLC2075392218 (DE-He213)BF02536831-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Gaetani, Maurizio verfasserin aut The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Paläontologie, Universität Erlangen 1989 Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) Gorza, Marta aut Enthalten in Facies Springer-Verlag, 1979 21(1989), 1 vom: Dez., Seite 41-56 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:21 year:1989 number:1 month:12 pages:41-56 https://doi.org/10.1007/BF02536831 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_285 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4305 AR 21 1989 1 12 41-56 |
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10.1007/BF02536831 doi (DE-627)OLC2075392218 (DE-He213)BF02536831-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Gaetani, Maurizio verfasserin aut The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Paläontologie, Universität Erlangen 1989 Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) Gorza, Marta aut Enthalten in Facies Springer-Verlag, 1979 21(1989), 1 vom: Dez., Seite 41-56 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:21 year:1989 number:1 month:12 pages:41-56 https://doi.org/10.1007/BF02536831 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_285 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4305 AR 21 1989 1 12 41-56 |
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10.1007/BF02536831 doi (DE-627)OLC2075392218 (DE-He213)BF02536831-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Gaetani, Maurizio verfasserin aut The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Paläontologie, Universität Erlangen 1989 Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) Gorza, Marta aut Enthalten in Facies Springer-Verlag, 1979 21(1989), 1 vom: Dez., Seite 41-56 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:21 year:1989 number:1 month:12 pages:41-56 https://doi.org/10.1007/BF02536831 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_285 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4305 AR 21 1989 1 12 41-56 |
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10.1007/BF02536831 doi (DE-627)OLC2075392218 (DE-He213)BF02536831-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Gaetani, Maurizio verfasserin aut The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Paläontologie, Universität Erlangen 1989 Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) Gorza, Marta aut Enthalten in Facies Springer-Verlag, 1979 21(1989), 1 vom: Dez., Seite 41-56 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:21 year:1989 number:1 month:12 pages:41-56 https://doi.org/10.1007/BF02536831 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_285 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4305 AR 21 1989 1 12 41-56 |
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10.1007/BF02536831 doi (DE-627)OLC2075392218 (DE-He213)BF02536831-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Gaetani, Maurizio verfasserin aut The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institut für Paläontologie, Universität Erlangen 1989 Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) Gorza, Marta aut Enthalten in Facies Springer-Verlag, 1979 21(1989), 1 vom: Dez., Seite 41-56 (DE-627)130281867 (DE-600)569234-9 (DE-576)015852024 0172-9179 nnns volume:21 year:1989 number:1 month:12 pages:41-56 https://doi.org/10.1007/BF02536831 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_285 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2027 GBV_ILN_2173 GBV_ILN_4012 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4305 AR 21 1989 1 12 41-56 |
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Enthalten in Facies 21(1989), 1 vom: Dez., Seite 41-56 volume:21 year:1989 number:1 month:12 pages:41-56 |
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Gaetani, Maurizio |
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550 VZ 13 ssgn The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) Paleontology Paleoecology Carbonatebank Lombardy (Italy) Anisian (Middle-Triassic) |
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The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) |
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The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) |
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Gaetani, Maurizio |
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1989 |
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Gaetani, Maurizio Gorza, Marta |
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the anisian (middle triassic) carbonate bank of camorelli (lombardy, southern alps) |
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The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) |
| abstract |
Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. © Institut für Paläontologie, Universität Erlangen 1989 |
| abstractGer |
Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. © Institut für Paläontologie, Universität Erlangen 1989 |
| abstract_unstemmed |
Summary During the Anisian (?Bithynian to Pelsonian) a large carbonate bank, up to 400 m thick, (the Camorelli Limestone) developed in the Lombardian Alps. Many stratigraphic sections were measured in this unit and three basic microfacies were detected, often arranged in sequence from bottom to top: intrabioclastic packstone, bindstone, and bioclastic packstone rich in Foraminifera. The biofacies is dominated by blue-green algae (Spongiostromata and Porostromata) and microproblematicTubiphytes. Benthic Foraminifera are subordinate even if they become locally the main bioclastic component. Dasycladacean algae are rare. These rather undifferentiated microfacies strongly contrast with time-equivalent mound microfacies, as previously pointed out for mounds versus large carbonate bank in the Illyrian. These features can be connected with substratum competition, not fully suitable for sponges in shallower environment at this stage of the Triassic recovering after the Late Permian crisis. © Institut für Paläontologie, Universität Erlangen 1989 |
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The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps) |
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