| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2015 |
| Язык | английский |
|
Арефьев Михаил Павлович, автор
Муравьев Федор Александрович, автор
Низамутдинов Назым Минсафович, автор
Силантьев Владимир Владимирович, автор
Хасанова Наиля Мидхатовна, автор
|
|
Трифонов Александр Андреевич, автор
|
| Библиографическое описание на языке оригинала |
Mouraviev, F. A. Red paleosols in the key sections of the Middle and Upper Permian of the Kazan Volga region and their paleoclimatic significance / F. A. Mouraviev, M. P. Arefiev, V. V. Silantiev, N. M. Khasanova, N. M. Nizamutdinov, and A. A. Trifonov // Paleontological Journal. - 2015. - Vol. 49. - № 10. - Р. 1150–1159. |
| Аннотация |
This paper presents the preliminary results of investigations of carbonate nodules from red paleo
sols of the reference sections of the Middle and Upper Permian of the Kazan Volga region. The main genetic
types of paleosols are calcic gleysols and gleyed vertisols, the pedogenic nodules are composed of dolomite
and calcite. Scanning electron microscopy and spectroscopic and isotopic methods of analysis show that the
nodules retained their original mineral composition and were formed with the participation of soil microor
ganisms under conditions of contrasting seasonality in an arid climate. In the vicinity of the Kiama?Illawarra
paleomagnetic boundary, the Urzhumian paleosols show a transition in the composition of pedogenic nod
ules from dolomite to calcite. It is suggested that this transition was caused by the humidization of climate,
which is supported by lithological and isotopic data |
| Ключевые слова |
paleosols, pedogenic nodules, Middle and Upper Permian, Kiama-Illawarra boundary, dolomite, calcite |
| Название журнала |
Paleontological journal
|
| URL |
http://link.springer.com/article/10.1134/S0031030115110064 |
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=118066 |
| Файлы ресурса | |
|
|
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Арефьев Михаил Павлович |
ru_RU |
| dc.contributor.author |
Муравьев Федор Александрович |
ru_RU |
| dc.contributor.author |
Низамутдинов Назым Минсафович |
ru_RU |
| dc.contributor.author |
Силантьев Владимир Владимирович |
ru_RU |
| dc.contributor.author |
Хасанова Наиля Мидхатовна |
ru_RU |
| dc.contributor.author |
Трифонов Александр Андреевич |
ru_RU |
| dc.date.accessioned |
2015-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2015-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2015 |
ru_RU |
| dc.identifier.citation |
Mouraviev, F. A. Red paleosols in the key sections of the Middle and Upper Permian of the Kazan Volga region and their paleoclimatic significance / F. A. Mouraviev, M. P. Arefiev, V. V. Silantiev, N. M. Khasanova, N. M. Nizamutdinov, and A. A. Trifonov // Paleontological Journal. - 2015. - Vol. 49. - № 10. - Р. 1150–1159. |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=118066 |
ru_RU |
| dc.description.abstract |
Paleontological journal |
ru_RU |
| dc.description.abstract |
This paper presents the preliminary results of investigations of carbonate nodules from red paleo
sols of the reference sections of the Middle and Upper Permian of the Kazan Volga region. The main genetic
types of paleosols are calcic gleysols and gleyed vertisols, the pedogenic nodules are composed of dolomite
and calcite. Scanning electron microscopy and spectroscopic and isotopic methods of analysis show that the
nodules retained their original mineral composition and were formed with the participation of soil microor
ganisms under conditions of contrasting seasonality in an arid climate. In the vicinity of the Kiama?Illawarra
paleomagnetic boundary, the Urzhumian paleosols show a transition in the composition of pedogenic nod
ules from dolomite to calcite. It is suggested that this transition was caused by the humidization of climate,
which is supported by lithological and isotopic data |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
paleosols |
ru_RU |
| dc.subject |
pedogenic nodules |
ru_RU |
| dc.subject |
Middle and Upper Permian |
ru_RU |
| dc.subject |
Kiama-Illawarra boundary |
ru_RU |
| dc.subject |
dolomite |
ru_RU |
| dc.subject |
calcite |
ru_RU |
| dc.title |
Red paleosols in the key sections of the Middle and Upper Permian of the Kazan Volga region and their paleoclimatic significance |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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