Vertical distribution of major, minor and trace elements in sediments from mud volcanoes of the Gulf of Cadiz: evidence of Cd, As and Ba fronts in upper layers
Autor: | C.L. Mieiro, Vitor Magalhães, Lina Carvalho, Rui Monteiro, Joana C. Almeida, Eduarda Pereira, Luis M. Pinheiro, Carlos Vale, Paula Figueira |
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Rok vydání: | 2018 |
Předmět: |
0106 biological sciences
010504 meteorology & atmospheric sciences 010604 marine biology & hydrobiology Geochemistry Sediment chemistry.chemical_element Barium Aquatic Science Oceanography 01 natural sciences Diagenesis chemistry Anaerobic oxidation of methane Transition zone Precipitation Loss on ignition Geology 0105 earth and related environmental sciences Mud volcano |
Zdroj: | Deep Sea Research Part I: Oceanographic Research Papers. 131:133-143 |
ISSN: | 0967-0637 |
DOI: | 10.1016/j.dsr.2017.12.003 |
Popis: | Mud volcanoes are feature of the coastal margins where anaerobic oxidation of methane triggers geochemical signals. Elemental composition, percentage of fine particles and loss on ignition were determined in sediment layers of eleven gravity cores retrieved from four mud volcanoes (Sagres, Bonjardim, Soloviev and Porto) and three undefined structures located on the deep Portuguese margin of the Gulf of Cadiz. Calcium was positively correlated to Sr and inversely to Al as well as to most of the trace elements. Vertical profiles of Ba, Cd and As concentrations, and their ratios to Al, in Porto and Soloviev showed pronounced enhancements in the top 50-cm depth. Sub-surface enhancements were less pronounced in other mud volcanoes and were absent in sediments from the structures. These profiles were interpreted as diagenetic enrichments related to the anaerobic oxidation of methane originated from upward methane-rich fluxes. The observed barium fronts were most likely caused by the presence of barite which precipitated at the sulphate-methane transition zone. Cd and As enrichments have probably resulted from successive dissolution/precipitation of sulphides in response to vertical shifts of redox boundaries. |
Databáze: | OpenAIRE |
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