Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores
| ISSN: |
1573-0417
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|---|---|
| Keywords: |
Lake Winnipeg ; plant macrofossils ; entomology ; AMS ; radiocarbon ; ‘hard-water’ effect
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| Source: |
Springer Online Journal Archives 1860-2000
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| Topics: |
Biology
Geosciences
|
| Notes: |
Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage.
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| Type of Medium: |
Electronic Resource
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| URL: |
| _version_ | 1798296527920168961 |
|---|---|
| autor | Vance, R. E. Telka, A. M. |
| autorsonst | Vance, R. E. Telka, A. M. |
| book_url | http://dx.doi.org/10.1023/A:1007994318477 |
| datenlieferant | nat_lic_papers |
| hauptsatz | hsatz_simple |
| identnr | NLM194859800 |
| issn | 1573-0417 |
| journal_name | Journal of paleolimnology |
| materialart | 1 |
| notes | Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage. |
| package_name | Springer |
| publikationsjahr_anzeige | 1998 |
| publikationsjahr_facette | 1998 |
| publikationsjahr_intervall | 8004:1995-1999 |
| publikationsjahr_sort | 1998 |
| publisher | Springer |
| reference | 19 (1998), S. 329-334 |
| schlagwort | Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect |
| search_space | articles |
| shingle_author_1 | Vance, R. E. Telka, A. M. |
| shingle_author_2 | Vance, R. E. Telka, A. M. |
| shingle_author_3 | Vance, R. E. Telka, A. M. |
| shingle_author_4 | Vance, R. E. Telka, A. M. |
| shingle_catch_all_1 | Vance, R. E. Telka, A. M. Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage. 1573-0417 15730417 Springer |
| shingle_catch_all_2 | Vance, R. E. Telka, A. M. Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage. 1573-0417 15730417 Springer |
| shingle_catch_all_3 | Vance, R. E. Telka, A. M. Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage. 1573-0417 15730417 Springer |
| shingle_catch_all_4 | Vance, R. E. Telka, A. M. Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Lake Winnipeg plant macrofossils entomology AMS radiocarbon ‘hard-water’ effect Abstract Conventional radiocarbon dating of Lake Winnipeg core samples has produced erroneously old ages due to the incorporation of pre-Quaternary carbon derived from carbonaceous rocks, soils and sediments in the watershed, as well as a ‘hard-water’ effect resulting from leaching of calcareous rocks and soils. To circumvent these problems and develop a reliable chronology for the Lake Winnipeg core series, a total of 64 samples from the Lake Winnipeg core series were processed to isolate well preserved macrofossils suitable for Accelerator Mass Spectrometry (AMS) radiocarbon dating. Here we report six radiocarbon ages derived from plant macrofossils and ostracodes, and reconstruct aspects of the depositional environment of each sample based on the associated macrofossil assemblage. 1573-0417 15730417 Springer |
| shingle_title_1 | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| shingle_title_2 | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| shingle_title_3 | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| shingle_title_4 | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| sigel_instance_filter | dkfz geomar wilbert ipn albert fhp |
| source_archive | Springer Online Journal Archives 1860-2000 |
| timestamp | 2024-05-06T09:53:31.285Z |
| titel | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| titel_suche | Accelerator mass spectrometry radiocarbon dating of 1994 Lake Winnipeg cores |
| topic | W TE-TZ |
| uid | nat_lic_papers_NLM194859800 |