Devonian Acid Sulfate Paleosol – First Finding on Central Devonian Field (Voronezh High, South Russia)

T. V. Alekseeva; Алексеева Т. В.; A. O. Alekseev; Алексеев А. О.

doi:10.1134/S0032180X24010027

Devonian Acid Sulfate Paleosol – First Finding on Central Devonian Field (Voronezh High, South Russia)

Авторлар: Alekseeva T.V.¹, Alekseev A.O.¹
Мекемелер:
1. Institute of Physical Chemical and Biological Problems of Soil Science of the Russian Academy of Sciences
Шығарылым: № 1 (2024)
Беттер: 14-26
Бөлім: ПАЛЕОПОЧВОВЕДЕНИЕ
URL: https://journals.rcsi.science/0032-180X/article/view/259355
DOI: https://doi.org/10.1134/S0032180X24010027
EDN: https://elibrary.ru/ZLSVNY
ID: 259355

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат
Рұқсат жабық

Рұқсат берілді
Рұқсат жабық

Тек жазылушылар үшін

Аннотация
Толық мәтін
Авторлар туралы
Әдебиет тізімі
Қосымша файлдар
Статистика

Аннотация

The paper presents the detail multidisciplinary study of middle Devonian (Eifelian) paleosol (PS) recently discovered on the territory of Voronezh Anteclise. The paleosol is developed from acid volcanic rock – rhyolitic tuff. The thickness of PS varies from 20 to 150 cm depending on the relief of Proterozoic basement beneath it. Tuff contains the inclusions of allochthonous coal particles, most part of each is substituted with pyrite. Main part of coal particles belongs to remnants of enigmatic biota – Nematophytes. The absence of rhizoliths and the microstructure of plant debris allowed to presume that PS was developed under primitive rootless vegetation. The paleosol formation is the result of predominantly chemical weathering. Its development was initiated by pyrite oxidation. PS demonstrates the following complex of pedological signs: kaolinite clay formation and redistribution, tongue bottom, Fe mobility, formation of Fe and gypsum containing nodules, in situ formation of kaolinite, gypsum, Fe-oxides, Fe-sulphates. Based on analytical data the discovered PS is attributed to acid sulphate soil. Deep transformation of parent rocks had the localized character and was not accompanied by formation of distinct soil horizons.

Негізгі сөздер

chemical weathering, rhyolite, pyrite, gypsum, Nematophytes

Толық мәтін

Авторлар туралы

T. Alekseeva

Institute of Physical Chemical and Biological Problems of Soil Science of the Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: alekseeva@issp.serpukhov.su
ORCID iD: 0000-0002-3880-2573
Ресей, Pushchino Moscow region, 142292

A. Alekseev

Institute of Physical Chemical and Biological Problems of Soil Science of the Russian Academy of Sciences

Email: alekseeva@issp.serpukhov.su
Ресей, Pushchino Moscow region, 142292

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