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Characteristics of Early Earth’s Critical Zone Based on Middle—Late Devonian Paleosol Properties (Voronezh High, Russia)

Published online by Cambridge University Press:  01 January 2024

Tatiana Alekseeva ,
Pavel Kabanov ,
Andrey Alekseev ,
Pavel Kalinin  and
Veronika Alekseeva
Tatiana Alekseeva*
Affiliation:
Institute of Physical, Chemical, and Biological Problems of Soil Science, Russian Academy of Sciences, ul. Institutskaya, 2, Pushchino, 142290, Russia
Pavel Kabanov
Affiliation:
Geological Survey of Canada, 3303 33rd Street N.W. Calgary, Alberta, Canada T2L 2A7
Andrey Alekseev
Affiliation:
Institute of Physical, Chemical, and Biological Problems of Soil Science, Russian Academy of Sciences, ul. Institutskaya, 2, Pushchino, 142290, Russia
Pavel Kalinin
Affiliation:
Institute of Physical, Chemical, and Biological Problems of Soil Science, Russian Academy of Sciences, ul. Institutskaya, 2, Pushchino, 142290, Russia
Veronika Alekseeva
Affiliation:
Faculty of Geography, Moscow State University, Leninskie Gori, Moscow 119999, Russia
*
*E-mail address of corresponding author: [email protected]
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Abstract

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Land colonization with vascular plants during the late Silurian—early Devonian and then arborescence during the Pragian—Givetian caused the development of new soil types. These true-rooted soils increased the rate of pedogenesis on a global scale. Since that time, soil has become a key component of the biosphere and has given rise to profound development of the Earth’s Critical Zone (CZ). Case studies of Devonian CZs have helped to record the transformation from Precambrian—Lower Paleozoic ‘proto-CZs,’ which had insufficient proto-soil cover, to modern soils with true-rooted pedosphere. Devonian (Givetian—Frasnian) paleosols from the Voronezh region of Russia are combined into pedocomplexes which occupied the top, slope, and bottom positions of a pronounced paleo-relief. Paleosols were developed from terrigenous argillites and volcanigenic-sedimentary deposits. Each pedocomplex consisted of four or more paleosols with different degrees of development and profile preservation. Paleosols exhibited several common characteristics including production and translocation of clay, ferruginization and the presence of siderite nodules, enhanced MnO/Al2O3 and (Fe2O{3}+MnO)/Al2O3 values, and in situ roots and root-system traces. The latter are siderite/goethite substituted. Stable isotope analysis of siderite shows δ13C values of between -6.1 and -13.7% indicating that CO2 had originated from C3 plants. The main mineral component of clay fractions in automorphic paleosols (top and slope of the paleorelief) is kaolinite. The important feature of these paleosols is the red-stained hematite-rich layer in their bases. These horizons developed at different depths and with different thicknesses, and marked the paleo-groundwater tables of each sub-CZ. Evidence of the imprints of vegetation is seen in the abundant in situ roots, plant fragments, and spores of rhyniophytes, lycopsids, progymnosperms, cladoxylalean ferns, and phytoleims of algae-like vascular plants. The near-equatorial location and the overall characteristics of paleosols studied suggest that the aforementioned horizons were formed in a tropically warm and humid climate. The paleo-ecological environments which accompanied pedogenesis were probably controlled by tectonic activity and volcanism.

Keywords

Central Devonian FieldClay MineralogyDevonian PaleosolsDevonian RootsMineral WeatheringPaleo-Critical ZoneVoronezh Anteclise
Type
Article
Information
Clays and Clay Minerals , Volume 64 , Issue 5 , October 2016 , pp. 677 - 694
Copyright
Copyright © Clay Minerals Society 2016

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