Relevant bibliographies by topics / Sea level eustasy

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Sea level eustasy'

Author: Grafiati
Published: 3 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Sea level eustasy"

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Sames, Benjamin, M. Wagreich, C. P. Conrad, and S. Iqbal. "Aquifer-eustasy as the main driver of short-term sea-level fluctuations during Cretaceous hothouse climate phases." Geological Society, London, Special Publications 498, no. 1 (2019): 9–38. http://dx.doi.org/10.1144/sp498-2019-105.

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AbstractA review of short-term (<3 myr: c. 100 kyr to 2.4 myr) Cretaceous sea-level fluctuations of several tens of metres indicates recent fundamental progress in understanding the underlying mechanisms for eustasy, both in timing and in correlation. Cretaceous third- and fourth-order hothouse sea-level changes, the sequence-stratigraphic framework, are linked to Milankovitch-type climate cycles, especially the longer-period sequence-building bands of 405 kyr and 1.2 myr. In the absence of continental ice sheets during Cretaceous hothouse phases (e.g. Cenomanian–Turonian), growing evidence
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Raymo, Maureen E., Jerry X. Mitrovica, Michael J. O’Leary, Robert M. DeConto, and Paul J. Hearty. "Departures from eustasy in Pliocene sea-level records." Nature Geoscience 4, no. 5 (2011): 328–32. http://dx.doi.org/10.1038/ngeo1118.

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Milne, Glenn A., and Jerry X. Mitrovica. "Searching for eustasy in deglacial sea-level histories." Quaternary Science Reviews 27, no. 25-26 (2008): 2292–302. http://dx.doi.org/10.1016/j.quascirev.2008.08.018.

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NEIGE, P., D. MARCHAND, and A. BONNOT. "Ammonoid morphological signal versus sea-level changes." Geological Magazine 134, no. 2 (1997): 261–64. http://dx.doi.org/10.1017/s0016756897006687.

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The morphological diversity, considered as a biological signal, of a series of four Upper Callovian (Middle Jurassic) ammonite populations of Côte-d’Or (France) is quantified. These populations fall within two third-order sequences of a second-order transgression. A sampling method that adheres as closely as possible to the morphological characteristics of the populations is established. It is valuable in that it eliminates the subjectivity related to taxonomy to allow more objective comparisons between the biological signal (shell morphology) and the physical signal (eustasy).
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Lin, Wen, Janok P. Bhattacharya, Brian R. Jicha, Brad S. Singer, and William Matthews. "Has Earth ever been ice-free? Implications for glacio-eustasy in the Cretaceous greenhouse age using high-resolution sequence stratigraphy." GSA Bulletin 133, no. 1-2 (2020): 243–52. http://dx.doi.org/10.1130/b35582.1.

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Abstract Controls on high-frequency sequences formed during super-greenhouse conditions in the Late Cretaceous Western Interior Seaway remain equivocal because of the active foreland basin tectonic setting and the lack of direct evidence of polar glaciations to support a glacio-eustatic origin. This paper quantifies eustatic sea-level changes based on high-resolution sequence stratigraphic analysis and improved chronometry of shallow marine deposits of the Late Cretaceous Gallup Sandstone in New Mexico, USA. Backstripping techniques remove tectonic and compactional subsidence and enable quanti
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Haq, Bilal U., and Abdul Motaleb Al-Qahtani. "Phanerozoic cycles of sea-level change on the Arabian Platform." GeoArabia 10, no. 2 (2005): 127–60. http://dx.doi.org/10.2113/geoarabia1002127.

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ABSTRACT The Arabian Plate has experienced a complex tectonic history while also being widely influenced by eustatic sea-level changes. These diastrophic events either affected changes in the rate and/or location of subsidence that in turn led to the creation of significant new sedimentary accommodation, or caused major erosional hiatuses. As a result, both eustasy and tectonics have played important roles in the development of sedimentary sequences and in determining the locus and characteristics of reservoir, source and seal facies on the Arabian Platform. Here, we present a synthesis (Cycle
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Li, Yifan, Xiaojie Wei, Kui Liu, and Kening Qi. "Sequence Stratigraphic and Geochemical Records of Paleo-Sea Level Changes in Upper Carboniferous Mixed Clastic–Carbonate Successions in the Eastern Qaidam Basin." Journal of Marine Science and Engineering 13, no. 7 (2025): 1299. https://doi.org/10.3390/jmse13071299.

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The Upper Carboniferous strata in the eastern Qaidam Basin, comprising several hundred meters of thick, mixed clastic–carbonate successions that have been little reported or explained, provide an excellent geological record of paleoenvironmental and paleo-sea level changes during the Late Carboniferous icehouse period. This tropical carbonate–clastic system offers critical constraints for correlating equatorial sea level responses with high-latitude glacial cycles during the Late Paleozoic Ice Age. Based on detailed outcrop observations and interpretations, five facies assemblages, including f
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Matthews, Robley K., and Moujahed I. Al-Husseini. "Orbital-forcing glacio-eustasy: A sequence-stratigraphic time scale." GeoArabia 15, no. 3 (2010): 155–67. http://dx.doi.org/10.2113/geoarabia1503155.

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ABSTRACT This essay provides further explanation of the mathematical details of orbital forcing and glacio-eustatic modeling (Parametric Forward Modeling, PFM) aspects and applications. A slight tune-up of the Earth’s eccentricity calculations (LA04 of Lasker et al., 2004) produces a near-perfect repeat of 14.58 million-year period and allows PFM to predict the glacio-eustatic component of sea-level fluctuation throughout the Phanerozoic. Generalities of an exploratory grid search of the parameter space of the model are reviewed and repetitive peak sea levels and low sea levels are noted in co
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Immenhauser, Adrian, and Robley K. Matthews. "Albian sea-level cycles in Oman: the ‘Rosetta Stone’ approach." GeoArabia 9, no. 3 (2004): 11–46. http://dx.doi.org/10.2113/geoarabia090311.

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ABSTRACT The Albian Nahr Umr Formation of Oman (bounded by the Shu’aiba and Natih formations) recorded high-, intermediate, and low-amplitude regressive-transgressive events. In order to reconstruct these sea-level oscillations in a semi-quantitative manner, six measured sections from different bathymetric positions were investigated across a 500-km-transect. Between these sections, discontinuity surfaces, indicative of sea-level fall and subsequent rise, were correlated. In order to asses the underlying causes of sea-level oscillations we compared the amplitudes and frequencies of the Oman ev
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Brikiatis, Leonidas. "Arido-eustasy: A new example of non-glacial eustatic sea level change." Gondwana Research 70 (June 2019): 25–35. http://dx.doi.org/10.1016/j.gr.2018.12.012.

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Dissertations / Theses on the topic "Sea level eustasy"

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Marshall, Paul. "Palaeoenvironmental, climatic and sea-level fluctuations and sequence stratigraphy of the Scottish Bathonian." Thesis, University of Aberdeen, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.325229.

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Books on the topic "Sea level eustasy"

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1929-, Dott Robert H., ed. Eustasy: The historical ups and downs of a major geological concept. Geological Society of America, 1992.

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David, Macdonald, ed. Sedimentation, tectonics, and eustasy: Sea-level changes at active margins. Blackwell Scientific Publications, 1991.

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L, Pindell James, and Drake Charles L, eds. Paleogeographic evolution and non-glacial eustasy, northern South America. SEPM (Society for Sedimentary Geology), 1998.

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Congrès, français de sédimentologie (2nd 1989 Paris France and Lyon France). Mesozoic eustacy record on western Tethyan margins: Book of abstracts. Association des sédimentologistes français, 1989.

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5

Ramkumar, Mu, and David Menier. Eustasy, High-Frequency Sea Level Cycles and Habitat Heterogeneity. Elsevier, 2017.

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Macdonald, David I. M. Sedimentation, Tectonics and Eustasy: Sea-Level Changes at Active Margins. Wiley & Sons, Incorporated, John, 2009.

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Macdonald, David I. M. Sedimentation, Tectonics and Eustasy: Sea-Level Changes at Active Margins. Wiley & Sons, Limited, John, 2009.

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8

Jr, Robert H. Dott. Eustasy: The Historical Ups and Downs of a Major Geological Concept (Memoir (Geological Society of America)). Geological Society of America, 1992.

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(Editor), James L. Pindell, and Charles Drake (Editor), eds. Paleogeographic Evolution and Non-Clacial Eustacy. Geological Society Publishing House, 1998.

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Mesozoic eustacy record on western Tethyan margins: Book of abstracts (Association des sedimentologistes francais). Association des sedimentologistes francais, 1989.

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Book chapters on the topic "Sea level eustasy"

1

Otvos, Ervin G. "Eustasy and Sea Level." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_364.

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Otvos, Ervin G. "Eustasy and Sea Level." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-48657-4_364-1.

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Otvos, Ervin G. "Eustasy and Sea Level." In Encyclopedia of Earth Sciences Series. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-48657-4_364-2.

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Sherman, Ian. "Holocene Sea-Level Changes and Crustal Movements in the North Sea Region: An Experiment with Regional Eustasy." In Late Quaternary Sea-Level Correlation and Applications. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0873-4_1.

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Soussi, Mohamed. "Phanerozoic Global Sea-Level Changes: Evidences from Tunisia Illustrating how Eduard Suess’ Concepts (Gondwana, Tethys, Eustasy) are Still Relevant." In Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_1.

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ST. C. KENDALL, CHRISTOPHER G., and IAN LERCHE. "THE RISE AND FALL OF EUSTASY." In Sea-Level Changes. SEPM (Society for Sedimentary Geology), 1988. http://dx.doi.org/10.2110/pec.88.01.0003.

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HALLAM, A. "A REEVALUATION OF JURASSIC EUSTASY IN THE LIGHT OF NEW DATA AND THE REVISED EXXON CURVE." In Sea-Level Changes. SEPM (Society for Sedimentary Geology), 1988. http://dx.doi.org/10.2110/pec.88.01.0261.

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Ramkumar, Mu, and David Menier. "Sequences, Sea-Level Cycles, and Habitat Dynamics." In Eustasy, High-Frequency Sea Level Cycles and Habitat Heterogeneity. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-812720-9.00002-4.

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Ramkumar, Mu, and David Menier. "Influence of Sea-Level on Facies and Habitat Heterogeneity." In Eustasy, High-Frequency Sea Level Cycles and Habitat Heterogeneity. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-812720-9.00003-6.

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Ramkumar, Mu, and David Menier. "Defining Habitat and Habitat Heterogeneity." In Eustasy, High-Frequency Sea Level Cycles and Habitat Heterogeneity. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-812720-9.00001-2.

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Conference papers on the topic "Sea level eustasy"

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Artyushkov, E. V. "Relative Sea–level Changes in Cratonic Basins–Tectonics or Eustasy." In Saint Petersburg 2010. EAGE Publications BV, 2010. http://dx.doi.org/10.3997/2214-4609.20145425.

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Jameson, Jeremy, and Christian J. Strohmenger. "Resolving Eustasy from Neotectonics in the Sea-Level History of the Pliocene to Holocene of Qatar." In International Petroleum Technology Conference. International Petroleum Technology Conference, 2014. http://dx.doi.org/10.2523/17219-ms.

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Jameson, Jeremy, and Christian J. Strohmenger. "Resolving Eustasy from Neotectonics in the Sea-Level History of the Pliocene to Holocene of Qatar." In International Petroleum Technology Conference. International Petroleum Technology Conference, 2014. http://dx.doi.org/10.2523/iptc-17219-ms.

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Jameson, J., and C. J. Strohmenger. "Resolving Eustasy from Neotectonics in the Sea-Level History of the Pliocene to Holocene of Qatar." In IPTC 2014: International Petroleum Technology Conference. European Association of Geoscientists & Engineers, 2014. http://dx.doi.org/10.3997/2214-4609-pdb.395.iptc-17219-ms.

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Polly, P. David. "EARTH SYSTEMS, EUSTASY, AND EVOLUTION: COMPUTATIONAL MODELING OF THE EFFECTS OF SEA LEVEL CHANGE ON TRAIT EVOLUTION AND MORPHOLOGICAL DISPARITY IN BERMUDAN LAND SNAILS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-280821.

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Kembuan, B. B. S. "TOC Prediction Using Delta Log Resistivity, and Its Distribution in Cyclostratigraphy-INPEFA Trend in “S-Field”, Kutai Basin”." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-sg-136.

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S field has unique geological conditions, with a depth of maturity around 800 meters based on geochemical analysis and classified as the shallowest in the Kutai Basin compared to other fields of around 4000 meters. This is caused by this field's geological conditions, which are influenced by the tectonic gravitational force from the north and the lifting of the middle Miocene formation from below. The study aims to have better understanding on the petroleum system using the ∆ Log R to analyse the source rock, to be integrated with the Cyclostratigraphy-INPEFA log to discover which cyclic depos
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