Calcareous sediments of the Muwaqqar Chalk Marl Formation, Jordan: Mineralogical and geochemical evidences for Zn and Cd enrichment

Calcareous sediments of the Muwaqqar Chalk Marl Formation, Jordan: Mineralogical and geochemical evidences for Zn and Cd enrichment Научная публикация

Журнал

Gondwana Research
ISSN: 1342-937X , E-ISSN: 1878-0571

Вых. Данные

Год: 2017, Том: 46, Страницы: 204-226 Страниц : 23 DOI: 10.1016/j.gr.2017.03.008

Ключевые слова

Muwaqqar Chalk Marl Formation; Organic-rich calcareous sediments; Anoxia; Redox sensitive elements; Mississippi Valley-type deposits

Авторы

Sokol Ella V. ¹ , Kozmenko Olga A. ¹ , Khoury Hani N. ² , Kokh Svetlana N. ¹ , Novikova Sofya A. ¹ , Nefedov Andrey A. ^3,4 , Sokol Ivan A. ¹ , Zaikin Pavel ³

Организации

1	(Данные Web of science) Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, 3 Koptyug Ave, Novosibirsk 630090, Russia
2	(Данные Web of science) Univ Jordan, Amman 11942, Jordan
3	(Данные Web of science) Russian Acad Sci, NN Vorozhtsov Novosibirsk Inst Organ Chem, Siberian Branch, 9 Lavrentiev Ave, Novosibirsk 630090, Russia
4	(Данные Web of science) Novosibirsk State Univ, Pirogov St 2, Novosibirsk 630090, Russia

Immature organic-rich siliceous chalk ('oil shale') and organic-poor limestones of the Maastrichtian-Paleocene Muwaqqar Chalk Marl Formation (MCM) (central Jordan) deposited on the southern Neo-Tethys epicontinental shelf provide a perfect example of carbonate sedimentation in a bioproductive upwelling environment. The MCM sediments have been studied by XRD, SEM, EMPA, sequential extraction, ICP-MS, GC-MS, and FTIR to gain in-sights into causes of their unusual composition. The sediments are remarkable by exceptionally high enrichment in phosphorus and redox sensitive elements (RSE), mainly Cd (up to 225 ppm), Zn (1500 ppm), and Mo (up to 180 ppm), as well as in Ni, V, Cr, and U, with a total RSE budget reaching 3200 ppm, coupled with up to 23 wt% organic matter and 4.3 wt% sulphur. The bulk organic matter consists of type I/II kerogens sulphurised during sulphate reduction. Redox sensitive metals were brought to sediments mainly by biogenic shuttle, while the terrestrial input was minor, and hydrothermal fluids apparently did not contribute to total RSE. The metals can reside in sulphide (Zn-Cd-(Cu)) in sphalerite or/and wurtzite; Fe-Ni-V-Cu-(Mo) in pyrite, carbonate (Zn-Cd-(Mo-Ni-V)), and organic (Ni-V-Cu) phases. Authigenic Cd-rich sphalerite and wurtzite are much more abundant than pyrite in immature 'oil shales', for three main reasons: (i) S-bearing ligands coordinating Cd and Zn in primary organic matter; (ii) high sulphur in organic matter; and (iii) low concentrations of reactive iron in bottom sediments. Limestones redeposited under oxic environments lose all sulphides, but high Zn (up to 337 ppm) and Cd (up to 29 ppm) become redistributed into the newly formed carbonates. Thus, shelf carbonates of different ages deposited under anoxic/sulfidic conditions in zones of high bioproductivity, as well as their derivative limestones and dolomites, can be the primary Zn and Cd storage for Mississippi Valley-type deposits with high Zn/Pb and Cd/Zn ratios. (C) 2017 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Sokol E.V. , Kozmenko O.A. , Khoury H.N. , Kokh S.N. , Novikova S.A. , Nefedov A.A. , Sokol I.A. , Zaikin P.
Calcareous sediments of the Muwaqqar Chalk Marl Formation, Jordan: Mineralogical and geochemical evidences for Zn and Cd enrichment
Gondwana Research. 2017. V.46. P.204-226. DOI: 10.1016/j.gr.2017.03.008 WOS Scopus

Опубликована в печати:

1 июн. 2017 г.

Web of science	WOS:000399985000013
Scopus	2-s2.0-85018476406
OpenAlex	W2601660828