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Discovery of a silicate rock-boring organism and macrobioerosion in fresh water. / Bolotov, Ivan N.; Aksenova, Olga V.; Bakken, Torkild; Glasby, Christopher J.; Gofarov, Mikhail Yu; Kondakov, Alexander V.; Konopleva, Ekaterina S.; Lopes-Lima, Manuel; Lyubas, Artyom A.; Wang, Yu; Bychkov, Andrey Yu; Sokolova, Agniya M.; Tanmuangpak, Kitti; Tumpeesuwan, Sakboworn; Vikhrev, Ilya V.; Shyu, J. Bruce H.; Win, Than; Pokrovsky, Oleg S.

в: Nature Communications, Том 9, № 1, 2882, 2018.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Bolotov, IN, Aksenova, OV, Bakken, T, Glasby, CJ, Gofarov, MY, Kondakov, AV, Konopleva, ES, Lopes-Lima, M, Lyubas, AA, Wang, Y, Bychkov, AY, Sokolova, AM, Tanmuangpak, K, Tumpeesuwan, S, Vikhrev, IV, Shyu, JBH, Win, T & Pokrovsky, OS 2018, 'Discovery of a silicate rock-boring organism and macrobioerosion in fresh water', Nature Communications, Том. 9, № 1, 2882. https://doi.org/10.1038/s41467-018-05133-4

APA

Bolotov, I. N., Aksenova, O. V., Bakken, T., Glasby, C. J., Gofarov, M. Y., Kondakov, A. V., Konopleva, E. S., Lopes-Lima, M., Lyubas, A. A., Wang, Y., Bychkov, A. Y., Sokolova, A. M., Tanmuangpak, K., Tumpeesuwan, S., Vikhrev, I. V., Shyu, J. B. H., Win, T., & Pokrovsky, O. S. (2018). Discovery of a silicate rock-boring organism and macrobioerosion in fresh water. Nature Communications, 9(1), [2882]. https://doi.org/10.1038/s41467-018-05133-4

Vancouver

Author

Bolotov, Ivan N. ; Aksenova, Olga V. ; Bakken, Torkild ; Glasby, Christopher J. ; Gofarov, Mikhail Yu ; Kondakov, Alexander V. ; Konopleva, Ekaterina S. ; Lopes-Lima, Manuel ; Lyubas, Artyom A. ; Wang, Yu ; Bychkov, Andrey Yu ; Sokolova, Agniya M. ; Tanmuangpak, Kitti ; Tumpeesuwan, Sakboworn ; Vikhrev, Ilya V. ; Shyu, J. Bruce H. ; Win, Than ; Pokrovsky, Oleg S. / Discovery of a silicate rock-boring organism and macrobioerosion in fresh water. в: Nature Communications. 2018 ; Том 9, № 1.

BibTeX

@article{655935cda76a4726b323c6d9282a24ce,
title = "Discovery of a silicate rock-boring organism and macrobioerosion in fresh water",
abstract = "Macrobioerosion is a common process in marine ecosystems. Many types of rock-boring organisms break down hard substrates, particularly carbonate rocks and calcareous structures such as dead corals and shells. In paleontology, the presence of rocks with boreholes and fossil macroboring assemblage members is one of the primary diagnostic features of shallow marine paleo-environments. Here we describe a silicate rock-boring organism and an associated community in submerged siltstone rock outcrops in Kaladan River, Myanmar. The rock-boring mussel Lignopholas fluminalis is a close relative of the marine piddocks, and its borings belong to the ichnospecies Gastrochaenolites anauchen. The neotectonic uplift of the area leading to gradual decrease of the sea level with subsequent shift from estuarine to freshwater environment was the most likely driver for the origin of this community. Our findings highlight that rocks with macroborings are not an exclusive indicator of marine paleo-ecosystems, but may also reflect freshwater habitats.",
author = "Bolotov, {Ivan N.} and Aksenova, {Olga V.} and Torkild Bakken and Glasby, {Christopher J.} and Gofarov, {Mikhail Yu} and Kondakov, {Alexander V.} and Konopleva, {Ekaterina S.} and Manuel Lopes-Lima and Lyubas, {Artyom A.} and Yu Wang and Bychkov, {Andrey Yu} and Sokolova, {Agniya M.} and Kitti Tanmuangpak and Sakboworn Tumpeesuwan and Vikhrev, {Ilya V.} and Shyu, {J. Bruce H.} and Than Win and Pokrovsky, {Oleg S.}",
year = "2018",
doi = "10.1038/s41467-018-05133-4",
language = "English",
volume = "9",
journal = "Nature Communications",
issn = "2041-1723",
publisher = "Nature Publishing Group",
number = "1",

}

RIS

TY - JOUR

T1 - Discovery of a silicate rock-boring organism and macrobioerosion in fresh water

AU - Bolotov, Ivan N.

AU - Aksenova, Olga V.

AU - Bakken, Torkild

AU - Glasby, Christopher J.

AU - Gofarov, Mikhail Yu

AU - Kondakov, Alexander V.

AU - Konopleva, Ekaterina S.

AU - Lopes-Lima, Manuel

AU - Lyubas, Artyom A.

AU - Wang, Yu

AU - Bychkov, Andrey Yu

AU - Sokolova, Agniya M.

AU - Tanmuangpak, Kitti

AU - Tumpeesuwan, Sakboworn

AU - Vikhrev, Ilya V.

AU - Shyu, J. Bruce H.

AU - Win, Than

AU - Pokrovsky, Oleg S.

PY - 2018

Y1 - 2018

N2 - Macrobioerosion is a common process in marine ecosystems. Many types of rock-boring organisms break down hard substrates, particularly carbonate rocks and calcareous structures such as dead corals and shells. In paleontology, the presence of rocks with boreholes and fossil macroboring assemblage members is one of the primary diagnostic features of shallow marine paleo-environments. Here we describe a silicate rock-boring organism and an associated community in submerged siltstone rock outcrops in Kaladan River, Myanmar. The rock-boring mussel Lignopholas fluminalis is a close relative of the marine piddocks, and its borings belong to the ichnospecies Gastrochaenolites anauchen. The neotectonic uplift of the area leading to gradual decrease of the sea level with subsequent shift from estuarine to freshwater environment was the most likely driver for the origin of this community. Our findings highlight that rocks with macroborings are not an exclusive indicator of marine paleo-ecosystems, but may also reflect freshwater habitats.

AB - Macrobioerosion is a common process in marine ecosystems. Many types of rock-boring organisms break down hard substrates, particularly carbonate rocks and calcareous structures such as dead corals and shells. In paleontology, the presence of rocks with boreholes and fossil macroboring assemblage members is one of the primary diagnostic features of shallow marine paleo-environments. Here we describe a silicate rock-boring organism and an associated community in submerged siltstone rock outcrops in Kaladan River, Myanmar. The rock-boring mussel Lignopholas fluminalis is a close relative of the marine piddocks, and its borings belong to the ichnospecies Gastrochaenolites anauchen. The neotectonic uplift of the area leading to gradual decrease of the sea level with subsequent shift from estuarine to freshwater environment was the most likely driver for the origin of this community. Our findings highlight that rocks with macroborings are not an exclusive indicator of marine paleo-ecosystems, but may also reflect freshwater habitats.

UR - http://www.scopus.com/inward/record.url?scp=85050595474&partnerID=8YFLogxK

U2 - 10.1038/s41467-018-05133-4

DO - 10.1038/s41467-018-05133-4

M3 - Article

C2 - 30038289

AN - SCOPUS:85050595474

VL - 9

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

IS - 1

M1 - 2882

ER -

ID: 47719660