Black Mn-Fe crusts as markers of abrupt palaeoenvironmental changes in El Soplao Cave (Cantabria, Spain)

International Journal of Speleology. 2011;40(2):163-169

 

Journal Homepage

Journal Title: International Journal of Speleology

ISSN: 0392-6672 (Print); 1827-806X (Online)

Publisher: Società Speleologica Italiana

LCC Subject Category: Science: Biology (General) | Science: Geology

Country of publisher: Italy

Language of fulltext: English

Full-text formats available: PDF

 

AUTHORS

Gazquez Fernando
Calaforra José Maria
Forti Paolo

EDITORIAL INFORMATION

Double blind peer review

Editorial Board

Instructions for authors

Time From Submission to Publication: 27 weeks

 

Abstract | Full Text

Peculiar iron and manganese deposits coating walls, floors and ceilings of many galleries are one of the special features of the ElSoplao Cave (Cantabria, Spain). These speleothems appear to have been deposited over wall clay deposits, as well as formingpart of flowstones. Structure of crusts is essentially amorphous but several manganese and iron oxides were identified like goethiteand birnessite, though all occur with a low degree of crystallinity. In the outer layer of the crusts, alteration iron minerals appear thatderive from previous minerals in a process probably mediated by microorganisms. EDX microanalyses report fairly high values of Feand Mn in the crusts, though the Mn/Fe ratio varies considerably as a function of distance from the substrate/bedrock. The presentstudy proposes a genetic model for crust speleothems in El Soplao, based on oscillations of the phreatic level. The origin of thesedeposits is related to mobilization, under phreatic conditions, of polymetallic sulfides in the host rock. Metal ions (including Fe²+ andMn²+) released into the cave under reducing conditions, are oxidized and fixed in a process mediated by bacteria, giving rise to oxidesand hydroxides of low crystallinity. The presence of various black intercalated layers in aragonite flowstones indicate periods whencave conditions suddenly changed from vadose, when aragonite is precipitated, to phreatic and epiphreatic conditions, when theMn-Fe deposits are precipitated. Subsequently, vadose conditions were re-established, leading to the final stages of precipitation ofaragonite recorded in the flowstone and recent aragonite helictites on the surface of the Mn-Fe crusts.