Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics

Valentin Krassilov; Sophia Barinova

doi:doi:10.11648/j.earth.20130201.11

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Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics

Valentin Krassilov, Sophia Barinova

Published in Earth Sciences (Volume 2, Issue 1)

Published: 20 February 2013

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Abstract

The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes

Published in	Earth Sciences (Volume 2, Issue 1)
DOI	10.11648/j.earth.20130201.11
Page(s)	1-8
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2013. Published by Science Publishing Group

Keywords

Sea level; Geomagnetic reversals; Rotation geodynamics; Geochronology

References

[1]	R.J. Huggett, "Fluvialism or diluvialism? Changing views on superfloods and landscape change". Progr. Phys. Geogr., vol. 18, pp. 335–342. September 1994.
[2]	V.A. Krassilov, Terrestrial Palaeoecology and Global Change. Sophia: Pensoft, 2003.
[3]	J.W. Snedden, C.A. Liu, "A compilation of Phanerozoic sea-level change, coastal onlaps and recommended sequence designations". Search and Discovery Article 40594. Ex-xonMobil Production Deutschland GmbH, 2010, www.searchanddiscovery.org.
[4]	J. Hardenbol, J. Thierry, M.B. Farley, T. Jacquin, P.C. Gra-ciansky, and P. Vail, "Mesozoic and Cenozoic sequence chronostratigraphic framework of European basins", In Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, P.C. Graciansky et al. Eds. SEPM Special Pub. no. 60, 1998, pp. 3–13.
[5]	B.U. Haq and Al-Qahtani, "Phanerozoic cycles of sea-level change on the Arabian Platform". GeoArabia, vol. 10, no. 2, pp.127–160, 2005.
[6]	B.U. Haq and S.R. Shutter, "A chronology of Paleozoic sea-level changes". Science, vol. 322, pp. 64–68, October 2008.
[7]	J.G. Ogg, G. Ogg, and F.M. Gradstein, Concise Geologic Time Scale. Cambridge: University Press, 2008.
[8]	M. Kono, "Palaeomagnetism and palaeointensity studies of Scottish Devonian volcanic rocks". Geophys J. Intern., vol. 56, no. 2, pp. 385–396, February 1979.
[9]	A. Delabroye, and M. Vecoli, "The end-Ordovician glaciation and the Hirnantian Stage: A global review and questions about Late Ordovician event stratigraphy". Earth-Sci. Rev., vol. 98, no. 3, pp. 269–282, 2010.
[10]	S. Finnegan, K. Bergmann, J.M. Eiler, D.S. Jones, D.A. Fike, I. Eisenman et al. "The magnitude and duration of Late Or-dovician–Early Silurian glaciation". Science, vol. 331, no. 6019, pp.903–906, February 2011.
[11]	C.G.A. Harrison, "Long term eustasy and epeirogeny in continents." In Sea-level Change, Geophysics Study Com-mittee, National Research Council, Ed. Washington D.C.: Academic Press, 1990, pp. 141–158.
[12]	D.M. Pechersky, "The geomagnetic field at the Paleo-zoic/Mesozoic and Mesozoic/Cenozoic boundaries and lower mantle plumes". Izvestiya, Phys. Solid Earth, vol. 43, no. 10, pp. 844–854, 2007.
[13]	E.V. Artyushkov and P.A. Chekhovich, "Mechanisms of sea-depth changes in Silurian epeiric basins of east Siberia". Russian Geol. Geophys., vol. 45, no 11, 1219–1236, 2004.
[14]	C.A. Sandberg, J.R. Morrow, and W. Ziegler, "Late Devonian sea-level changes, catastrophic events, and mass extinctions". Geol. Soc. Amer. Spec. Paper, 356, pp. 356-473, 2002.
[15]	N.-A. Mörner, "Eustatic changes during the last 300 years. Palaeogeogr. Palaeoclim. Palaeoecol., vol. 13, no. 1, pp. 1–14, March 1973.
[16]	N.-A. Mörner, "Eustasy and geoid changes as a function of core/mantle changes". In Earth Rheology, Isostasy and Eustasy, N.-A. Mörner, Ed. N. Y.: Wiley, 1980, pp.535–553.
[17]	N.-A. Mörner, "The concept of eustasy: a redefinition". J. Coastal Res. Special issues 1, pp. 49–51, 1986.
[18]	N.-A. Mörner, "Models of global sea level changes". In Sea level Changes, M.J. Tooley and I. Shennan, Eds. Oxford: Blackwell, 1987a, pp. 333–355.
[19]	N.-A. Mörner, "Eustasy, geoid changes and dynamic sea surface changes due to the interchange of momentum". In Late Quaternary Sea-Level Changes, Y. Quin and S. Zhao, Eds. Beijing: China Ocean Press, 1987b, pp. 26–39.
[20]	N.-A. Mörner, "Sea-level changes and Earth's rate of rotation". J. Coastal Res., vol. 8, no. 4, pp. 966–971, Autumn, 1992.
[21]	V.A. Krassilov, Plate tectonics and rotational dynamics of the planet. Izvestia Acad. Sci. U.S.S.R, Geol., no. 1, pp. 74–82, 1976. (В.А. Красилов, "Тектоника плит и ротационный режим планеты", Известия Акад. Наук СССР, сер. Геол. № 1, С. 74-82, 1976).
[22]	V.A. Krassilov, "Organic evolution and natural stratigraphical classification". Lethaia , vol. 11, no. 2, pp. 93–104, April 1978.
[23]	V.A. Krassilov, Cretaceous Period. Evolution of Earth Crust and Biosphere. Moscow; Nauka, 1985. (В.А. Красилов, Меловой период. Эволюция земной коры и биосферы. Москва: Наука, 1985).
[24]	V.A. Krassilov, "Overview of rotational geodynamics", Pacific Geology, no. 1. pp. 89–95, April 1991. (В.А. Красилов, "Обзор ротационной геодинамики" Тихоок. Геол., № 1, С. 89–95, 1991).
[25]	G.A. Glatzmaier and P.H. Roberts, "A three-dimensional self-consistent computer simulation of a geomagnetic field reversal", Nature, vol. 377, pp. 203–209, 21 September 1995.
[26]	G.A. Glatzmaier and P.H. Roberts, "Rotation and magnetism of Earth's inner core’, Science, vol. 274, no. 5294, pp. 1887–1891, December 1996.
[27]	P.L. Olson, G.A. Glatzmaier, and R. Coe, 2011. "Complex polarity reversals in a geodynamo model", Earth Planet. Sci. Let., vol. 304, pp.168–179, April 2011.

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Valentin Krassilov, Sophia Barinova. (2013). Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sciences, 2(1), 1-8. https://doi.org/10.11648/j.earth.20130201.11

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ACS Style

Valentin Krassilov; Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013, 2(1), 1-8. doi: 10.11648/j.earth.20130201.11

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AMA Style

Valentin Krassilov, Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013;2(1):1-8. doi: 10.11648/j.earth.20130201.11

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@article{10.11648/j.earth.20130201.11,
  author = {Valentin Krassilov and Sophia Barinova},
  title = {Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics},
  journal = {Earth Sciences},
  volume = {2},
  number = {1},
  pages = {1-8},
  doi = {10.11648/j.earth.20130201.11},
  url = {https://doi.org/10.11648/j.earth.20130201.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20130201.11},
  abstract = {The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes},
 year = {2013}
}

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TY  - JOUR
T1  - Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics
AU  - Valentin Krassilov
AU  - Sophia Barinova
Y1  - 2013/02/20
PY  - 2013
N1  - https://doi.org/10.11648/j.earth.20130201.11
DO  - 10.11648/j.earth.20130201.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 1
EP  - 8
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20130201.11
AB  - The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes
VL  - 2
IS  - 1
ER  -

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Author Information

Valentin Krassilov

Inst. of Evolution, University of Haifa, Haifa, Israel
Sophia Barinova

Inst. of Evolution, University of Haifa, Haifa, Israel

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Valentin Krassilov, Sophia Barinova. (2013). Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sciences, 2(1), 1-8. https://doi.org/10.11648/j.earth.20130201.11

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ACS Style

Valentin Krassilov; Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013, 2(1), 1-8. doi: 10.11648/j.earth.20130201.11

Copy | Download

AMA Style

Valentin Krassilov, Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013;2(1):1-8. doi: 10.11648/j.earth.20130201.11

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@article{10.11648/j.earth.20130201.11,
  author = {Valentin Krassilov and Sophia Barinova},
  title = {Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics},
  journal = {Earth Sciences},
  volume = {2},
  number = {1},
  pages = {1-8},
  doi = {10.11648/j.earth.20130201.11},
  url = {https://doi.org/10.11648/j.earth.20130201.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20130201.11},
  abstract = {The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes},
 year = {2013}
}

Copy | Download

TY  - JOUR
T1  - Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics
AU  - Valentin Krassilov
AU  - Sophia Barinova
Y1  - 2013/02/20
PY  - 2013
N1  - https://doi.org/10.11648/j.earth.20130201.11
DO  - 10.11648/j.earth.20130201.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 1
EP  - 8
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20130201.11
AB  - The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes
VL  - 2
IS  - 1
ER  -

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