Geochemistry of surface sediments from the northwestern Gulf of Mexico : implications for provenance and heavy metal contamination

Armstrong-Altrin, John S.; Botello, Alfonso V.; Villanueva, Susana F.; Soto, Luis A.

doi:10.7306/gq.1484

Artykuł - szczegóły

Tytuł artykułu

Geochemistry of surface sediments from the northwestern Gulf of Mexico : implications for provenance and heavy metal contamination

Autorzy

Armstrong-Altrin John S. , Botello Alfonso V. , Villanueva Susana F. , Soto Luis A.

Treść / Zawartość

Pełne teksty:

Armstrong_J_Geochemistry_GQ_Vol.63_No.3_2019.pdf

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Identyfikatory

DOI

10.7306/gq.1484

Warianty tytułu

Języki publikacji

Abstrakty

Thirty-five near-surface sediment samples were recovered from the continental shelf and upper slope regions of the north-western (NW) Gulf of Mexico. The geochemical data of the sediments recovered were examined to investigate the weathering intensity, provenance, palaeo-oxygenation condition, and level of heavy metal contamination. The sediments analysed showed a moderate to high intensity of chemical weathering. Major and trace element concentrations indicated a terrigenous origin, closely related to the weathering of rocks rich in aluminosilicates. The results of this study further revealed that major rivers, the Bravo and Soto La Marina, played an important role in delivering sediments to the study area. The concentration of transition trace elements such as Cr, Cu, Ni, and V revealed that the sediments were derived from intermediate rocks such as andesite. The V/Cr, Ni/Co, and Cu/Zn ratios in the sediments were <2, <5, and <1, respectively, suggesting a depositional process occurred under well-oxygenated conditions. Principle Component Analysis (PCA) did not show a significant difference in sediment texture between the continental shelf and slope areas. The enrichment factor (EF) and Geo-accumulation index (l_geo) values were <2 and <1, respectively, suggesting the absence of an anthropogenic input.

Słowa kluczowe

Tamaulipas deep-sea sediments enrichment factor contamination principle component analysis

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2019

Tom

Vol. 63, No. 3

Strony

522--538

Opis fizyczny

Bibliogr. 116 poz., rys., tab., wykr.

Twórcy

autor

Armstrong-Altrin John S.

armstrong@cmarl.unam.mx

Universidad Nacional Autónoma de México, Instituto de Ciencias del Mar y Limnología, Unidad de Procesos Oceánicos y Costeros, Circuito Exterior s/n, 04510 CDMX., México

autor

Botello Alfonso V.

Universidad Nacional Autónoma de México, Instituto de Ciencias del Mar y Limnología, Unidad de Procesos Oceánicos y Costeros, Circuito Exterior s/n, 04510 CDMX., México

autor

Villanueva Susana F.

Universidad Nacional Autónoma de México, Instituto de Ciencias del Mar y Limnología, Unidad de Procesos Oceánicos y Costeros, Circuito Exterior s/n, 04510 CDMX., México

autor

Soto Luis A.

Universidad Nacional Autónoma de México, Instituto de Ciencias del Mar y Limnología, Unidad de Procesos Oceánicos y Costeros, Circuito Exterior s/n, 04510 CDMX., México

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Uwagi

Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020).

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Bibliografia

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