Biogeochemical processes in canga ecosystems: Armoring of iron ore against erosion and importance in iron duricrust restoration in Brazil

被引:38
作者
Gagen, Emma J. [1 ]
Levett, Alan [1 ]
Paz, Anat [1 ]
Gastauer, Markus [2 ]
Caldeira, Cecilio Frois [2 ]
da Silva Valadares, Rafael Borges [2 ]
Pires Bitencourt, Jose Augusto [2 ]
Alves, Ronnie [2 ]
Oliveira, Guilherme [2 ]
Siqueira, Jose Oswaldo [2 ]
Vasconcelos, Paulo M. [1 ]
Southam, Gordon [1 ]
机构
[1] Univ Queensland, Sch Earth & Environm Sci, St Lucia, Qld 4072, Australia
[2] Inst Tecnol Vale, BR-66055090 Belem, Para, Brazil
基金
澳大利亚研究理事会;
关键词
Canga; Geomicrobiology; Iron cycling; Biogeochemistry; MINAS-GERAIS; QUADRILATERO-FERRIFERO; IRONSTONE OUTCROPS; OXIDIZING BACTERIA; COSMOGENIC HE-3; PLANT-COMMUNITIES; PLAQUE-FORMATION; EVOLUTION; GOETHITE; (U-TH)/HE;
D O I
10.1016/j.oregeorev.2019.03.013
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Supergene enriched iron ore deposits in Brazil are typically blanketed by goethite-cemented breccias that form a protective duricrust known as canga. Moderately hard, well consolidated, permeable and resistant to erosion and chemical weathering, the canga blanket protects the relatively friable iron ore below. The protective canga horizons in the Carajas and Quadrilatero Ferrffero mineral provinces represent some of the longest-lived, continuously exposed land surfaces on Earth, and their formation is essential to supergene iron ore enrichment and preservation. Remarkably, the iron-rich duricrusts that have developed in Brazilian tropical rainforest environments, i.e, Carajas, yield geochronological results that indicate that these ancient erosion-resistant surfaces continue to evolve today. Active biogeochemical iron cycling is essential for the 'self-healing' cementation/recementation occurring in canga, suggesting that recurrent iron reduction and subsequent oxidation are responsible for canga evolution. Macroscopic biological features in canga including ferruginised plant roots and termite tracks have been linked to the biogeochemical cycling of iron. The 'organic' textures in canga can be traced to the microscopic scale, preserving fossilised bacterial cell envelopes and permineralised biofilms. At the canga surface, naturally rare and endemic rupestrian plant species carve out an existence, commonly in the absence of soil. Growth of grasses also promotes metal cycling highlighting that the rhizosphere contributes to canga evolution. The fossilisation of microbial biofilms and rhizosphere horizons consolidates canga, affecting its permeability, limiting water transport and enhancing biogeochemical cycling. The development of canga has been essential for the formation, preservation, and discovery of iron ore deposits, and its restoration will ultimately be required for mined land remediation of these unique ecosystems.
引用
收藏
页码:573 / 586
页数:14
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