Spectral Analysis of Late Pleistocene-Holocene Sediments
Abstract Spectral analysis of deep-sea sediments indicates that the fluctuations in compositional parameters are not random fluctuations with time. Spectra show significant peaks representing periodicities in the data of 380, 1300, and 2600 years. Two of these periods are similar to periods reported...
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Cambridge University Press (CUP)
1973
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crcambridgeupr:10.1016/0033-5894(73)90050-1 2024-10-13T14:09:20+00:00 Spectral Analysis of Late Pleistocene-Holocene Sediments Pisias, Nicklas G. Dauphin, J.Paul Sancetta, Constance 1973 http://dx.doi.org/10.1016/0033-5894(73)90050-1 http://api.elsevier.com/content/article/PII:0033589473900501?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589473900501?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400035742 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 3, issue 1, page 3-9 ISSN 0033-5894 1096-0287 journal-article 1973 crcambridgeupr https://doi.org/10.1016/0033-5894(73)90050-1 2024-09-25T04:03:02Z Abstract Spectral analysis of deep-sea sediments indicates that the fluctuations in compositional parameters are not random fluctuations with time. Spectra show significant peaks representing periodicities in the data of 380, 1300, and 2600 years. Two of these periods are similar to periods reported in 14 C fluctuations. Analysis of a paleotemperature curve from the North Atlantic shows that the characteristics of the fluctuations within interglacial and glacial stages of the climate are similar, and that the spectrum has a significant peak at 2600 years. Article in Journal/Newspaper North Atlantic Cambridge University Press Quaternary Research 3 1 3 9 |
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Open Polar |
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Cambridge University Press |
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English |
description |
Abstract Spectral analysis of deep-sea sediments indicates that the fluctuations in compositional parameters are not random fluctuations with time. Spectra show significant peaks representing periodicities in the data of 380, 1300, and 2600 years. Two of these periods are similar to periods reported in 14 C fluctuations. Analysis of a paleotemperature curve from the North Atlantic shows that the characteristics of the fluctuations within interglacial and glacial stages of the climate are similar, and that the spectrum has a significant peak at 2600 years. |
format |
Article in Journal/Newspaper |
author |
Pisias, Nicklas G. Dauphin, J.Paul Sancetta, Constance |
spellingShingle |
Pisias, Nicklas G. Dauphin, J.Paul Sancetta, Constance Spectral Analysis of Late Pleistocene-Holocene Sediments |
author_facet |
Pisias, Nicklas G. Dauphin, J.Paul Sancetta, Constance |
author_sort |
Pisias, Nicklas G. |
title |
Spectral Analysis of Late Pleistocene-Holocene Sediments |
title_short |
Spectral Analysis of Late Pleistocene-Holocene Sediments |
title_full |
Spectral Analysis of Late Pleistocene-Holocene Sediments |
title_fullStr |
Spectral Analysis of Late Pleistocene-Holocene Sediments |
title_full_unstemmed |
Spectral Analysis of Late Pleistocene-Holocene Sediments |
title_sort |
spectral analysis of late pleistocene-holocene sediments |
publisher |
Cambridge University Press (CUP) |
publishDate |
1973 |
url |
http://dx.doi.org/10.1016/0033-5894(73)90050-1 http://api.elsevier.com/content/article/PII:0033589473900501?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589473900501?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400035742 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Quaternary Research volume 3, issue 1, page 3-9 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/0033-5894(73)90050-1 |
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Quaternary Research |
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3 |
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9 |
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1812816245254258688 |