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The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons. / Кичко, Арина Александровна; Sergaliev, Nurlan H.; Иванова, Екатерина Андреевна; Chernov, Timofey; Кимеклис, Анастасия Кирилловна; Орлова, Ольга Владимировна; Kalmenov, Murat; Akhmedenov, Kazmurat; Пинаев, Александр Георгиевич; Проворов, Николай Александрович; Шашков, Николай; Андронов, Евгений Евгеньевич.

в: Heliyon, Том 9, № 6, e17208, 12.06.2023.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Кичко, АА, Sergaliev, NH, Иванова, ЕА, Chernov, T, Кимеклис, АК, Орлова, ОВ, Kalmenov, M, Akhmedenov, K, Пинаев, АГ, Проворов, НА, Шашков, Н & Андронов, ЕЕ 2023, 'The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons', Heliyon, Том. 9, № 6, e17208. https://doi.org/10.1016/j.heliyon.2023.e17208

APA

Кичко, А. А., Sergaliev, N. H., Иванова, Е. А., Chernov, T., Кимеклис, А. К., Орлова, О. В., Kalmenov, M., Akhmedenov, K., Пинаев, А. Г., Проворов, Н. А., Шашков, Н., & Андронов, Е. Е. (2023). The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons. Heliyon, 9(6), [e17208]. https://doi.org/10.1016/j.heliyon.2023.e17208

Vancouver

Author

Кичко, Арина Александровна ; Sergaliev, Nurlan H. ; Иванова, Екатерина Андреевна ; Chernov, Timofey ; Кимеклис, Анастасия Кирилловна ; Орлова, Ольга Владимировна ; Kalmenov, Murat ; Akhmedenov, Kazmurat ; Пинаев, Александр Георгиевич ; Проворов, Николай Александрович ; Шашков, Николай ; Андронов, Евгений Евгеньевич. / The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons. в: Heliyon. 2023 ; Том 9, № 6.

BibTeX

@article{9d6138bd10de494e8176891129a7497a,
title = "The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons",
abstract = "Burial mounds represent a challenge for microbiologists. Could ancient buried soils preserve microbiomes as they do archaeological artifacts? To investigate this question, we studied the soil microbiome under a burial mound dating from 2500 years ago in Western Kazakhstan. Two soil profile cuts were established: one under the burial mound and another adjacent to the mound surface steppe soil. Both soils represented the same dark chestnut soil type and had the same horizontal stratification (A, B, C horizons) with slight alterations. DNA samples isolated from all horizons were studied with molecular techniques including qPCR and high throughput sequencing of amplicon libraries of the 16S rRNA gene fragment. The taxonomic structure of the microbiome of the buried horizons demonstrated a deep divergence from ones of the surface, comparable to the variation between different soil types (representatives of the soil types were included in the survey). The cause of this divergence could be attributed to diagenetic processes characterized by the reduction of organic matter content and changes in its structure. Corresponding trends in the microbiome structure are obvious from the beta-diversity pattern: the A and B horizons of the buried soils form one cluster with the C horizons of both buried and surface soil. This trend could generally be designated as 'mineralization'. Statistically significant changes between the buried and surface soils microbiomes were detected in the number of phylogenetic clusters, the biology of which is in the line of diagenesis. The trend of 'mineralization' was also supported by PICRUSt2 functional prediction, demonstrating a higher occurrence of the processes of degradation in the buried microbiome. Our results show a profound shift in the buried microbiome relatively the {"}surface{"} microbiome, indicating the deep difference between the original and buried microbiomes.",
keywords = "16s rRNA, Burial mound, Dark-chestnut soil, Diagenesis, High throughput sequencing, Kurgan, Microbiome",
author = "Кичко, {Арина Александровна} and Sergaliev, {Nurlan H.} and Иванова, {Екатерина Андреевна} and Timofey Chernov and Кимеклис, {Анастасия Кирилловна} and Орлова, {Ольга Владимировна} and Murat Kalmenov and Kazmurat Akhmedenov and Пинаев, {Александр Георгиевич} and Проворов, {Николай Александрович} and Николай Шашков and Андронов, {Евгений Евгеньевич}",
year = "2023",
month = jun,
day = "12",
doi = "10.1016/j.heliyon.2023.e17208",
language = "English",
volume = "9",
journal = "Heliyon",
issn = "2405-8440",
publisher = "Elsevier",
number = "6",

}

RIS

TY - JOUR

T1 - The microbiome of buried soils demonstrates significant shifts in taxonomic structure and a general trend towards mineral horizons

AU - Кичко, Арина Александровна

AU - Sergaliev, Nurlan H.

AU - Иванова, Екатерина Андреевна

AU - Chernov, Timofey

AU - Кимеклис, Анастасия Кирилловна

AU - Орлова, Ольга Владимировна

AU - Kalmenov, Murat

AU - Akhmedenov, Kazmurat

AU - Пинаев, Александр Георгиевич

AU - Проворов, Николай Александрович

AU - Шашков, Николай

AU - Андронов, Евгений Евгеньевич

PY - 2023/6/12

Y1 - 2023/6/12

N2 - Burial mounds represent a challenge for microbiologists. Could ancient buried soils preserve microbiomes as they do archaeological artifacts? To investigate this question, we studied the soil microbiome under a burial mound dating from 2500 years ago in Western Kazakhstan. Two soil profile cuts were established: one under the burial mound and another adjacent to the mound surface steppe soil. Both soils represented the same dark chestnut soil type and had the same horizontal stratification (A, B, C horizons) with slight alterations. DNA samples isolated from all horizons were studied with molecular techniques including qPCR and high throughput sequencing of amplicon libraries of the 16S rRNA gene fragment. The taxonomic structure of the microbiome of the buried horizons demonstrated a deep divergence from ones of the surface, comparable to the variation between different soil types (representatives of the soil types were included in the survey). The cause of this divergence could be attributed to diagenetic processes characterized by the reduction of organic matter content and changes in its structure. Corresponding trends in the microbiome structure are obvious from the beta-diversity pattern: the A and B horizons of the buried soils form one cluster with the C horizons of both buried and surface soil. This trend could generally be designated as 'mineralization'. Statistically significant changes between the buried and surface soils microbiomes were detected in the number of phylogenetic clusters, the biology of which is in the line of diagenesis. The trend of 'mineralization' was also supported by PICRUSt2 functional prediction, demonstrating a higher occurrence of the processes of degradation in the buried microbiome. Our results show a profound shift in the buried microbiome relatively the "surface" microbiome, indicating the deep difference between the original and buried microbiomes.

AB - Burial mounds represent a challenge for microbiologists. Could ancient buried soils preserve microbiomes as they do archaeological artifacts? To investigate this question, we studied the soil microbiome under a burial mound dating from 2500 years ago in Western Kazakhstan. Two soil profile cuts were established: one under the burial mound and another adjacent to the mound surface steppe soil. Both soils represented the same dark chestnut soil type and had the same horizontal stratification (A, B, C horizons) with slight alterations. DNA samples isolated from all horizons were studied with molecular techniques including qPCR and high throughput sequencing of amplicon libraries of the 16S rRNA gene fragment. The taxonomic structure of the microbiome of the buried horizons demonstrated a deep divergence from ones of the surface, comparable to the variation between different soil types (representatives of the soil types were included in the survey). The cause of this divergence could be attributed to diagenetic processes characterized by the reduction of organic matter content and changes in its structure. Corresponding trends in the microbiome structure are obvious from the beta-diversity pattern: the A and B horizons of the buried soils form one cluster with the C horizons of both buried and surface soil. This trend could generally be designated as 'mineralization'. Statistically significant changes between the buried and surface soils microbiomes were detected in the number of phylogenetic clusters, the biology of which is in the line of diagenesis. The trend of 'mineralization' was also supported by PICRUSt2 functional prediction, demonstrating a higher occurrence of the processes of degradation in the buried microbiome. Our results show a profound shift in the buried microbiome relatively the "surface" microbiome, indicating the deep difference between the original and buried microbiomes.

KW - 16s rRNA

KW - Burial mound

KW - Dark-chestnut soil

KW - Diagenesis

KW - High throughput sequencing

KW - Kurgan

KW - Microbiome

UR - https://www.mendeley.com/catalogue/0b1cb5cd-683f-35b8-9c98-b8abc3fb9a38/

U2 - 10.1016/j.heliyon.2023.e17208

DO - 10.1016/j.heliyon.2023.e17208

M3 - Article

C2 - 37360114

VL - 9

JO - Heliyon

JF - Heliyon

SN - 2405-8440

IS - 6

M1 - e17208

ER -

ID: 106508979