A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr
[Display omitted] •Ages of 89 major geological events during last 260 Myr.•Fourier analysis shows spectral peak at 27.5 Myr.•A significant shorter period of ~ 9 Myr to 10 Myr.•Global geologic activity in pulses with an underlying ~ 27.5-Myr cycle. We performed spectral analyses on the ages of 89 wel...
Gespeichert in:
Veröffentlicht in: | Di xue qian yuan. 2021-11, Vol.12 (6), p.101245, Article 101245 |
---|---|
Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | |
---|---|
container_issue | 6 |
container_start_page | 101245 |
container_title | Di xue qian yuan. |
container_volume | 12 |
creator | Rampino, Michael R. Caldeira, Ken Zhu, Yuhong |
description | [Display omitted]
•Ages of 89 major geological events during last 260 Myr.•Fourier analysis shows spectral peak at 27.5 Myr.•A significant shorter period of ~ 9 Myr to 10 Myr.•Global geologic activity in pulses with an underlying ~ 27.5-Myr cycle.
We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth’s motions in the Solar System and the Galaxy. |
doi_str_mv | 10.1016/j.gsf.2021.101245 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2621590968</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S1674987121001092</els_id><sourcerecordid>2621590968</sourcerecordid><originalsourceid>FETCH-LOGICAL-c368t-2d5264e7ec7c3dfa4a84732842076ec6456e274e6df85ada4cc751446fb9347b3</originalsourceid><addsrcrecordid>eNp9kEtOwzAQhi0EElXpAdhZYp1iO47twKqqykMqYgNry7UnqaMQFzup1NtwFk5GSlkzm9FI_2P0IXRNyZwSKm6beZ2qOSOMHm_GizM0YYVSWUlLdo4mVEielUrSSzRLqSHjSKmkJBPkF3g3tAlwqHC_Bbwysd_e4QVmcl5kL4eIh85BbA--q7E92Baw77ANITrfmR4criG0ofbWtBj20PUJhz3E37DWpB4zQb6_xqArdFGZsWn2t6fo_WH1tnzK1q-Pz8vFOrO5UH3GXMEEBwlW2txVhhvFZc4UZ0QKsIIXApjkIFylCuMMt1YWlHNRbcqcy00-RTen3F0MnwOkXjdhiN1YqZlgtChJKdSooieVjSGlCJXeRf9h4kFToo9QdaNHqPoIVZ-gjp77kwfG9_ceok7WQ2fB-Qi21y74f9w_wRJ9pw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2621590968</pqid></control><display><type>article</type><title>A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr</title><source>Elsevier ScienceDirect Journals</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>Rampino, Michael R. ; Caldeira, Ken ; Zhu, Yuhong</creator><creatorcontrib>Rampino, Michael R. ; Caldeira, Ken ; Zhu, Yuhong</creatorcontrib><description>[Display omitted]
•Ages of 89 major geological events during last 260 Myr.•Fourier analysis shows spectral peak at 27.5 Myr.•A significant shorter period of ~ 9 Myr to 10 Myr.•Global geologic activity in pulses with an underlying ~ 27.5-Myr cycle.
We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth’s motions in the Solar System and the Galaxy.</description><identifier>ISSN: 1674-9871</identifier><identifier>EISSN: 2588-9192</identifier><identifier>DOI: 10.1016/j.gsf.2021.101245</identifier><language>eng</language><publisher>Oxford: Elsevier B.V</publisher><subject>Basalt ; Celestial bodies ; Confidence intervals ; Correlations ; Cyclic pulses ; Fourier analysis ; Geology ; Global geological events ; Ocean floor ; Plate tectonics ; Plates (tectonics) ; Sea level ; Tectonics</subject><ispartof>Di xue qian yuan., 2021-11, Vol.12 (6), p.101245, Article 101245</ispartof><rights>2021 China University of Geosciences (Beijing) and Peking University</rights><rights>Copyright Elsevier Science Ltd. Nov 2021</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c368t-2d5264e7ec7c3dfa4a84732842076ec6456e274e6df85ada4cc751446fb9347b3</citedby><cites>FETCH-LOGICAL-c368t-2d5264e7ec7c3dfa4a84732842076ec6456e274e6df85ada4cc751446fb9347b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.gsf.2021.101245$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>314,777,781,3537,27905,27906,45976</link.rule.ids></links><search><creatorcontrib>Rampino, Michael R.</creatorcontrib><creatorcontrib>Caldeira, Ken</creatorcontrib><creatorcontrib>Zhu, Yuhong</creatorcontrib><title>A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr</title><title>Di xue qian yuan.</title><description>[Display omitted]
•Ages of 89 major geological events during last 260 Myr.•Fourier analysis shows spectral peak at 27.5 Myr.•A significant shorter period of ~ 9 Myr to 10 Myr.•Global geologic activity in pulses with an underlying ~ 27.5-Myr cycle.
We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth’s motions in the Solar System and the Galaxy.</description><subject>Basalt</subject><subject>Celestial bodies</subject><subject>Confidence intervals</subject><subject>Correlations</subject><subject>Cyclic pulses</subject><subject>Fourier analysis</subject><subject>Geology</subject><subject>Global geological events</subject><subject>Ocean floor</subject><subject>Plate tectonics</subject><subject>Plates (tectonics)</subject><subject>Sea level</subject><subject>Tectonics</subject><issn>1674-9871</issn><issn>2588-9192</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kEtOwzAQhi0EElXpAdhZYp1iO47twKqqykMqYgNry7UnqaMQFzup1NtwFk5GSlkzm9FI_2P0IXRNyZwSKm6beZ2qOSOMHm_GizM0YYVSWUlLdo4mVEielUrSSzRLqSHjSKmkJBPkF3g3tAlwqHC_Bbwysd_e4QVmcl5kL4eIh85BbA--q7E92Baw77ANITrfmR4criG0ofbWtBj20PUJhz3E37DWpB4zQb6_xqArdFGZsWn2t6fo_WH1tnzK1q-Pz8vFOrO5UH3GXMEEBwlW2txVhhvFZc4UZ0QKsIIXApjkIFylCuMMt1YWlHNRbcqcy00-RTen3F0MnwOkXjdhiN1YqZlgtChJKdSooieVjSGlCJXeRf9h4kFToo9QdaNHqPoIVZ-gjp77kwfG9_ceok7WQ2fB-Qi21y74f9w_wRJ9pw</recordid><startdate>202111</startdate><enddate>202111</enddate><creator>Rampino, Michael R.</creator><creator>Caldeira, Ken</creator><creator>Zhu, Yuhong</creator><general>Elsevier B.V</general><general>Elsevier Science Ltd</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>202111</creationdate><title>A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr</title><author>Rampino, Michael R. ; Caldeira, Ken ; Zhu, Yuhong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c368t-2d5264e7ec7c3dfa4a84732842076ec6456e274e6df85ada4cc751446fb9347b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Basalt</topic><topic>Celestial bodies</topic><topic>Confidence intervals</topic><topic>Correlations</topic><topic>Cyclic pulses</topic><topic>Fourier analysis</topic><topic>Geology</topic><topic>Global geological events</topic><topic>Ocean floor</topic><topic>Plate tectonics</topic><topic>Plates (tectonics)</topic><topic>Sea level</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rampino, Michael R.</creatorcontrib><creatorcontrib>Caldeira, Ken</creatorcontrib><creatorcontrib>Zhu, Yuhong</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Di xue qian yuan.</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rampino, Michael R.</au><au>Caldeira, Ken</au><au>Zhu, Yuhong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr</atitle><jtitle>Di xue qian yuan.</jtitle><date>2021-11</date><risdate>2021</risdate><volume>12</volume><issue>6</issue><spage>101245</spage><pages>101245-</pages><artnum>101245</artnum><issn>1674-9871</issn><eissn>2588-9192</eissn><abstract>[Display omitted]
•Ages of 89 major geological events during last 260 Myr.•Fourier analysis shows spectral peak at 27.5 Myr.•A significant shorter period of ~ 9 Myr to 10 Myr.•Global geologic activity in pulses with an underlying ~ 27.5-Myr cycle.
We performed spectral analyses on the ages of 89 well-dated major geological events of the last 260 Myr from the recent geologic literature. These events include times of marine and non-marine extinctions, major ocean-anoxic events, continental flood-basalt eruptions, sea-level fluctuations, global pulses of intraplate magmatism, and times of changes in seafloor-spreading rates and plate reorganizations. The aggregate of all 89 events shows ten clusters in the last 260 Myr, spaced at an average interval of ~ 26.9 Myr, and Fourier analysis of the data yields a spectral peak at 27.5 Myr at the ≥ 96% confidence level. A shorter period of ~ 8.9 Myr may also be significant in modulating the timing of geologic events. Our results suggest that global geologic events are generally correlated, and seem to come in pulses with an underlying ~ 27.5-Myr cycle. These cyclic pulses of tectonics and climate change may be the result of geophysical processes related to the dynamics of plate tectonics and mantle plumes, or might alternatively be paced by astronomical cycles associated with the Earth’s motions in the Solar System and the Galaxy.</abstract><cop>Oxford</cop><pub>Elsevier B.V</pub><doi>10.1016/j.gsf.2021.101245</doi><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1674-9871 |
ispartof | Di xue qian yuan., 2021-11, Vol.12 (6), p.101245, Article 101245 |
issn | 1674-9871 2588-9192 |
language | eng |
recordid | cdi_proquest_journals_2621590968 |
source | Elsevier ScienceDirect Journals; EZB-FREE-00999 freely available EZB journals |
subjects | Basalt Celestial bodies Confidence intervals Correlations Cyclic pulses Fourier analysis Geology Global geological events Ocean floor Plate tectonics Plates (tectonics) Sea level Tectonics |
title | A pulse of the Earth: A 27.5-Myr underlying cycle in coordinated geological events over the last 260 Myr |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-17T23%3A22%3A12IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20pulse%20of%20the%20Earth:%20A%2027.5-Myr%20underlying%20cycle%20in%20coordinated%20geological%20events%20over%20the%20last%20260%C2%A0Myr&rft.jtitle=Di%20xue%20qian%20yuan.&rft.au=Rampino,%20Michael%20R.&rft.date=2021-11&rft.volume=12&rft.issue=6&rft.spage=101245&rft.pages=101245-&rft.artnum=101245&rft.issn=1674-9871&rft.eissn=2588-9192&rft_id=info:doi/10.1016/j.gsf.2021.101245&rft_dat=%3Cproquest_cross%3E2621590968%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2621590968&rft_id=info:pmid/&rft_els_id=S1674987121001092&rfr_iscdi=true |