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Straits and seaways : controls, processes and implications in modern and ancient systems (2023)

Rossi, Valentina Marzia [HerausgeberIn] ; Longhitano,Sergio G. [HerausgeberIn] ; Olariu, Cornel [HerausgeberIn] ; [et al.]

London : The Geological Society

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Call number: 10.1144/SP523

In: Special publications / the Geological Society, London, Volume 523

Description / Table of Contents: Straits & seaways are the key features that connect oceans, seas & lakes. They regulate water, sediment & biota exchanges, & influence local & global climate. A good understanding of the evolution of straits & seaways is therefore fundamental to accurately reconstruct the palaeogeography, tectonics, palaeoecology & stratigraphy of interconnected basins, the climate dynamics of Earth's past as well as to exploit conventional & renewable energy resources. This volume provides a collection of articles dealing with both ancient & modern case studies, bringing together different but complementary disciplines, such as marine geology, process sedimentology & stratigraphy. With the contents encompassing the evolution, geomorphology, stratigraphy, sedimentology, oceanography & palaeogeography of straits & seaways, & their influence on climate, the book will be of interest to Earth scientists

Type of Medium: 12

Pages: 1 Online-Ressource (vi, 530 Seiten) , Illustrationen, Diagramme, Karten

ISBN: 178620570X , 9781786205704 , 978-1-78620-570-4

Series Statement: Special publications / the Geological Society, London 523

URL: https://doi.org/10.1144/SP523

Language: English

Note: Title description Full Access22 March 2023 About this title - Straits and Seaways: Controls, Processes and Implications in Modern and Ancient Systems V. M. Rossi, S. G. Longhitano, C. Olariu, and F. L. Chiocci https://doi.org/10.1144/SP523 Introduction Full Access20 January 2023 Straits and seaways: controls, processes and implications in modern and ancient systems Valentina Marzia Rossi, Sergio G. Longhitano, Cornel Olariu, and Francesco L. Chiocci https://doi.org/10.1144/SP523-2022-271 Articles Open Access8 March 2022 A review of the morphology, physical processes and deposits of modern straits Robert W. Dalrymple https://doi.org/10.1144/SP523-2021-76 Open Access11 January 2023 Straits and seaways: end members within the continuous spectrum of the dynamic connection between basins Valentina Marzia Rossi, Sergio G. Longhitano, Cornel Olariu, and Francesco L. Chiocci https://doi.org/10.1144/SP523-2022-159 Full Access3 February 2022 The dire straits of Paratethys: gateways to the anoxic giant of Eurasia Dan V. Palcu and Wout Krijgsman https://doi.org/10.1144/SP523-2021-73 Full Access20 January 2022 The opening and closure of oceanic seaways during the Cenozoic: pacemaker of global climate change? André Bahr, Stefanie Kaboth-Bahr, and Cyrus Karas https://doi.org/10.1144/SP523-2021-54 Open Access7 December 2022 A shallow-water dunefield in a microtidal, wind-dominated strait (Stintino, NW Sardinia, Italy) S. Andreucci, A. Santonastaso, M. De Luca, S. Cappucci, A. Cucco, G. Quattrocchi, and V. Pascucci https://doi.org/10.1144/SP523-2021-188 Full Access17 October 2022 Bedforms of Bonifacio Strait (Western Mediterranean): hydrodynamics, coastal outline, supply and sediment distribution Giacomo Deiana, Valentino Demurtas, and Paolo Emanuele Orrù https://doi.org/10.1144/SP523-2022-10 Full Access20 January 2022 Morphology and Late Pleistocene–Holocene sedimentation of the Strait of Istanbul (Bosphorus): a review M. Namık Çağatay, K. Kadir Eriş, and Zeynep Erdem https://doi.org/10.1144/SP523-2021-48 Full Access27 January 2022 Large- and medium-scale morphosedimentary features of the Messina Strait: insights into bottom-current-controlled sedimentation and interaction with downslope processes E. Martorelli, D. Casalbore, F. Falcini, A. Bosman, F. G. Falese, and F. L. Chiocci https://doi.org/10.1144/SP523-2021-77 Full Access8 December 2022 Grain-size analysis of the Late Pleistocene sediments in the Corinth Rift: insights into strait-influenced hydrodynamics and provenance of an active rift basin Wenjun Kang, Shunli Li, Robert L. Gawthorpe, Mary Ford, Richard E. Ll. Collier, Xinghe Yu, Liliane Janikian, Casey W. Nixon, Romain Hemelsdaël, Spyros Sergiou, Jack Gillespie,... https://doi.org/10.1144/SP523-2022-166 Full Access26 April 2022 Stratigraphic architecture, sedimentology and structure of the Middle Pleistocene Corinth Canal (Greece) Basile Caterina, Romain Rubi, and Aurélia Hubert-Ferrari https://doi.org/10.1144/SP523-2021-143 Full Access18 May 2022 Channel, dune and sand sheet architectures of a strait-adjacent delta, Rifian Corridor, Morocco Daan Beelen, Lesli Joy Wood, Mohamed Najib Zaghloul, Sebastian Cardona, and Michiel Arts https://doi.org/10.1144/SP523-2021-49 Open Access11 October 2022 A new interpretation for the Pliensbachian Cook Formation (northern North Sea) as north–south-prograding tidal deltas and shelf ridges in the Early Jurassic Seaway: new model of linkage to the Norwegian Sea Atle Folkestad and Ronald J. Steel https://doi.org/10.1144/SP523-2021-75 Full Access17 January 2022 Early Pliocene marine transgression into the lower Colorado River valley, southwestern USA, by re-flooding of a former tidal strait Rebecca J. Dorsey, Juan Carlos Braga, Kevin Gardner, Kristin McDougall, and Brennan O'Connell https://doi.org/10.1144/SP523-2021-57 Full Access20 May 2022 Palaeostrait tectonosedimentary facies during late Cenozoic microplate rifting and dispersal in the western Mediterranean William Cavazza and Sergio G. Longhitano https://doi.org/10.1144/SP523-2021-95 Full Access8 March 2022 Sedimentary dynamics and topographic controls on the tidal-dominated Zagra Strait, Early Tortonian, Betic Cordillera, Spain Ángel Puga-Bernabéu, Juan Carlos Braga, Julio Aguirre, and José Manuel Martín https://doi.org/10.1144/SP523-2021-85 Full Access26 January 2022 Tectonic control on the palaeogeographical evolution of the Miocene Seaway along the Western Alpine foreland basin Amir Kalifi, Philippe Sorrel, Philippe-Hervé Leloup, Albert Galy, Vincenzo Spina, Bastien Huet, Séverine Russo, Bernard Pittet, and Jean-Loup Rubino https://doi.org/10.1144/SP523-2021-78 Full Access28 November 2022 Facies partitioning of fluvial, wave, and tidal influences across the shoreline-to-shelf architecture in the Western Interior Campanian Seaway, USA Keith P. Minor, Anton Wroblewski, Ronald J. Steel, Cornel Olariu, and Jeff P. Crabaugh https://doi.org/10.1144/SP523-2022-11

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Straits and seaways : controls, processes and implications in modern and ancient systems (2023)

Rossi, Valentina Marzia [HerausgeberIn] ; Longhitano,Sergio G. [HerausgeberIn] ; Olariu, Cornel [HerausgeberIn] ; [et al.]

London : The Geological Society

Associated volumes

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Details Availability

Call number: 9/M 07.0421(523)

In: Special publications / the Geological Society, London, Volume 523

Type of Medium: Monograph available for loan

Pages: vi, 530 Seiten , Illustrationen, Diagramme, Karten

ISBN: 178620570X , 9781786205704 , 978-1-78620-570-4

Series Statement: Special publications / the Geological Society, London 523

URL: https://doi.org/10.1144/SP523

Language: English

Location: Reading room

Branch Library: GFZ Library

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Submarine gullies on Italian upper slopes and their relationship with volcanic activity revisited 20 years after Bill Normark’s pioneering work (2011)

Chiocci, Francesco Latino ; Casalbore, Daniele

Geological Society of America (GSA)

In: Geosphere 7: 1284-1293.

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Publication Date: 2011-12-01

Description: Multibeam bathymetry and high-resolution seismic profiles depict in detail the characteristics of submarine gullies present in the upper continental slope offshore of the mouths of the Tiber and Volturno Rivers in the Tyrrhenian Sea and the Simeto River in the Ionian Sea. Upper slope gullies are interpreted as depositional features, growing because of faster aggradation on intergully areas with respect to their axes. The dispersal of river-flood sediment through plunging of hyperpycnal flows has been interpreted to be the limiting factor in sedimentation in gully axes. However, the generation of hyperpycnal flows requires a sediment concentration of several tens of kilograms per cubic meter in the river flows to overcome the higher density of seawater. This threshold is difficult to reach in medium-sized rivers (i.e., catchment basin of 500–5000 km2), such as the Tiber and Volturno. Two alternative scenarios of enhanced sediment availability for these rivers have been proposed. The first scenario is related to sea-level fall and lowstand stages, when the climate conditions may have been different and a huge amount of unconsolidated, fine-grained sediment deposited during the previous highstand stage may have been eroded from the river valleys, coastal plain valleys and shelf delta, as suggested in pioneering work of one of the authors (Chiocci) and Bill Normark. This scenario might explain the formation of some of the gullies offshore of the Tiber River mouth, which developed during the last glacial maximum; however, it is unable to explain the gullies within deposits related to transgressive and highstand system tracts, such as offshore of the Simeto and Volturno River mouths. An alternative scenario is thus proposed on the basis of the relationship observed between the studied rivers and the presence of large volcanic edifices in their catchment basins. Explosive volcanic activity could have drastically modified their catchment basins and caused a sudden and large supply of loose tephras, increasing the sediment load in watercourses and consequently favoring the development of gully-forming hyperpycnal flows. The timing of volcanic activity on the three study areas matches, in fact, the presence or absence of gullies in upper slope depositional sequences.

Electronic ISSN: 1553-040X

Topics: Geosciences