Cenozoic microfossils in northern Finland: Local reworking or distant wind transport?
Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hall, Adrian M. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013transfer abstract |
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| Umfang: |
14 |
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| Übergeordnetes Werk: |
Enthalten in: The head constituent plays a key role in the lexical boost in syntactic priming - Huang, Jian ELSEVIER, 2023, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:388 ; year:2013 ; day:15 ; month:10 ; pages:1-14 ; extent:14 |
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| DOI / URN: |
10.1016/j.palaeo.2013.07.012 |
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| 520 | |a Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. | ||
| 520 | |a Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. | ||
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10.1016/j.palaeo.2013.07.012 doi GBVA2013022000026.pica (DE-627)ELV027689239 (ELSEVIER)S0031-0182(13)00333-7 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? 2013transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Ebert, Karin oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:388 year:2013 day:15 month:10 pages:1-14 extent:14 https://doi.org/10.1016/j.palaeo.2013.07.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 388 2013 15 1015 1-14 14 045F 550 |
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10.1016/j.palaeo.2013.07.012 doi GBVA2013022000026.pica (DE-627)ELV027689239 (ELSEVIER)S0031-0182(13)00333-7 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? 2013transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Ebert, Karin oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:388 year:2013 day:15 month:10 pages:1-14 extent:14 https://doi.org/10.1016/j.palaeo.2013.07.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 388 2013 15 1015 1-14 14 045F 550 |
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10.1016/j.palaeo.2013.07.012 doi GBVA2013022000026.pica (DE-627)ELV027689239 (ELSEVIER)S0031-0182(13)00333-7 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? 2013transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Ebert, Karin oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:388 year:2013 day:15 month:10 pages:1-14 extent:14 https://doi.org/10.1016/j.palaeo.2013.07.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 388 2013 15 1015 1-14 14 045F 550 |
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10.1016/j.palaeo.2013.07.012 doi GBVA2013022000026.pica (DE-627)ELV027689239 (ELSEVIER)S0031-0182(13)00333-7 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? 2013transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Ebert, Karin oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:388 year:2013 day:15 month:10 pages:1-14 extent:14 https://doi.org/10.1016/j.palaeo.2013.07.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 388 2013 15 1015 1-14 14 045F 550 |
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10.1016/j.palaeo.2013.07.012 doi GBVA2013022000026.pica (DE-627)ELV027689239 (ELSEVIER)S0031-0182(13)00333-7 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? 2013transfer abstract 14 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. Ebert, Karin oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:388 year:2013 day:15 month:10 pages:1-14 extent:14 https://doi.org/10.1016/j.palaeo.2013.07.012 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 388 2013 15 1015 1-14 14 045F 550 |
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Cenozoic microfossils in northern Finland: Local reworking or distant wind transport? |
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Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. |
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Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. |
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Allochthonous Cenozoic microfossils have been reported from Late Pleistocene lake and mire host sediments across an area of >30,000km2 in northern Finland. Two main groups of microfossils are recognised: Palaeogene marine diatoms, silicoflagellates and ebridians that include taxa from around the time of the Palaeocene–Eocene Thermal Maximum and Pliocene to early Pleistocene freshwater diatoms. The presence of these microfossils has been regarded as evidence that Eocene marine and late Neogene freshwater sediments formerly existed on the shield surface. Both groups have been referred to frequently in reconstructions of the sea level, tectonic and erosion history of the northern Fennoscandian shield. The questions raised by the presence of allochthonous Cenozoic microfossils in northern Finland are, however, strongly resonant of the debate over the biota, origin and age of the Pliocene Sirius Group in Antarctica where competing hypotheses have been put forward of local deposition and reworking versus distant wind transport of marine diatoms from the continental shelf. |
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