Browsing by Author "Kaminski, Michael A."
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Item type:Article, Access status: Open Access , A new agglutinated foraminiferal species (Arenoturrispirillina waskowskae sp. nov.) from the Danian of Contessa, Italy(Wydawnictwa AGH, 2022) Hikmahtiar, Syouma; Kaminski, Michael A.This paper describes a new Paleogene deep-water agglutinated foraminifera from the Contessa Highway Section, Umbria-Marche Basin, Italy. The new species <i>Arenoturrispirillina waskowskae</i> is characterised by its predominently high trochospiral coiling, which distinguishes it from the genus Glomospira. The new species is also found in the Polish Carpathians.Item type:Article, Access status: Open Access , An Entzia-dominated marsh-type agglutinated foraminiferal assemblage from a salt marsh in Tubli Bay, Bahrain(Wydawnictwa AGH, 2020) Kaminski, Michael A.; Amao, Abduljamiu O.; Garrison, Thomas F.; Fiorini, Flavia; Magliveras, Simeon; Tawabini, Bassam S.; Waśkowska, AnnaA salt-marsh assemblage of agglutinated foraminifera was recovered from a salt marsh on the east side of Tubli Bay in eastern Bahrain. This locality is one of the last remaining patches of salt marsh on the east coast of Tubli Bay. The salt marsh is covered by a single marsh plant species, <i>Arthrocnemum macrostachyum</i>. Samples were collected from beneath the <i>Arthrocnemum</i> canopy in two transects beginning at the maximum landward extent of halophytic plants in the high marsh and extending to a tidal channel at the seaward side of the low marsh. A distinct elevation-related zonation in foraminifera is observed from the high marsh to the low marsh. The trochamminids <i>Entzia macrescens</i> and <i>Trochammina inflata</i> are characteristic of the high marsh, whereas <i>Ammonia</i>, <i>Elphidium</i>, <i>Peneroplis</i> and smaller miliolids become common in the middle part of the marsh transect. The tidal channel at the lower limit of the marsh contains an assemblage dominated by <i>Ammonia</i>, <i>Elphidium</i>, adult specimens of <i>Peneroplis</i>, and smaller miliolids, with <i>Clavulina</i> and <i>Agglutinella</i> as the only agglutinated taxa. Living specimens of <i>Entzia</i> and <i>Trochammina</i> were observed during the winter 2019–2020 sampling season, whereas samples collected in Autumn 2019 contained only dead specimens. One new species, <i>?Sigmoilina canisdementis</i> sp. nov., is described herein. This is the first report of a live <i>Entzia</i>-dominated salt marsh assemblage in the Arabian Gulf region.Item type:Article, Access status: Open Access , The Paleozoic formations of the Al Qassim Province in Saudi Arabia as potential sites for geotourism(Wydawnictwa AGH, 2019) Kaminski, Michael A.; Garrison, Thomas F.; Yoder, Carl E.The Paleozoic formations in the Middle East contain some of the world’s richest petroleum deposits, as they include excellent source and reservoir rocks. The Paleozoic rocks were deposited on the northern continental shelf of the Gondwanan continent at relatively high latitudes, and provide evidence of the Late Ordovician glacial event and associated sea-level changes. They also contain unique fossil remains. The Paleozoic formations exposed in the Al-Qassim province in Saudi Arabia are well-suited to become important sites for geotourism. Because the sedimentary formations are well-exposed and are easily accessible, they have strong capacity for development as tourist destinations. In this paper, we describe eight localities and their significance as potential educational sites for geology and palaeontology, as well as the archeological and economic significance of the Paleozoic formations of Saudi Arabia. The cultural and tourist infrastructure is summarised and a two-day field excursion is proposed.Item type:Article, Access status: Open Access , The White Volcanoes of Harrat Khaybar, north of Al-Madinah(2014) Kaminski, Michael A.; Al-Shaibani, Abdulaziz; Al-Ramadan, KhalidThe volcanic field of Harrat Khaybar north of Al-Madinah, Saudi Arabia contains rare examples of white volcanoes comprised mainly of the felsic rock comendite. The obsidian that occurs in association with the white comendite was exploited and worked by Neolithic inhabitants of the area. The white volcanoes are surrounded by more recent black basaltic lava fields that follow the pre-existing topography and display both aa and pahoehoe flow structures. Although situated only 60 km from a busy motorway, the volcanic area is remote and all necessary safety precautions must be taken in order to visit the volcanoes.
