Novel biomineralization strategy in calcareous foraminifera
Source at https://doi.org/10.1038/s41598-018-28400-2 . Licensed CC BY-NC-ND 4.0. This work shows that calcareous benthic foraminifera are capable of agglutinating sedimentary particles also. In particular, we focus on Melonis barleeanus. Traditionally considered a calcareous species, our data reveal...
Published in: | Scientific Reports |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Publishing Group
2018
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/13472 https://doi.org/10.1038/s41598-018-28400-2 |
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author | Borrelli, Chiara Panieri, Giuliana Dahl, Trine Merete Neufeld, Kai |
author_facet | Borrelli, Chiara Panieri, Giuliana Dahl, Trine Merete Neufeld, Kai |
author_sort | Borrelli, Chiara |
collection | University of Tromsø: Munin Open Research Archive |
container_issue | 1 |
container_title | Scientific Reports |
container_volume | 8 |
description | Source at https://doi.org/10.1038/s41598-018-28400-2 . Licensed CC BY-NC-ND 4.0. This work shows that calcareous benthic foraminifera are capable of agglutinating sedimentary particles also. In particular, we focus on Melonis barleeanus. Traditionally considered a calcareous species, our data revealed the presence of minute (~3 μm) sedimentary particles (silicate grains) inside the chamber walls of the examined shells. These particles were arranged in a definitive and systematic pattern, and the similar grain chemical characterization and size suggested a relatively high degree of selectivity in both modern and fossil specimens. Based on these results, we propose that M. barleeanus is capable of agglutinating sedimentary particles during the formation of a new chamber. The analysis of other calcareous foraminiferal species (e.g., Cassidulina neoteretis, Lobatula lobatula, Nonionella stella) did not reveal the presence of silicate grains in the shell of the specimens analyzed confirming this to be a characteristic of M. barleeanus. Considering that the isotopic and chemical composition of this species is widely used in paleoclimatic and paleoceanographic reconstructions, we used a mixing model to better constrain the influence of sedimentary particles on M. barleeanus δ 18 O data. Our model showed that the calcite δ 18 O would increase by ~0.9–2‰ if 10 wt% of feldspars (i.e., anorthite, albite, orthoclase) and quartz, respectively, were included in the analyzed shell. Based on these results, we emphasize that it is of paramount importance to consider M. barleeanus unusual biomineralization strategy during the interpretation of geological records and to investigate the presence of similar processes in other calcareous foraminiferal species. |
format | Article in Journal/Newspaper |
genre | Arctic |
genre_facet | Arctic |
geographic | Stella |
geographic_facet | Stella |
id | ftunivtroemsoe:oai:munin.uit.no:10037/13472 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-64.254,-64.254,-65.249,-65.249) |
op_collection_id | ftunivtroemsoe |
op_doi | https://doi.org/10.1038/s41598-018-28400-2 |
op_relation | Scientific Reports info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ info:eu-repo/grantAgreement/RCN/PETROMAKS2/255150/Norway/Norwegian margin fluid systems and methane- derived carbonate crusts - Recent scientific advances in service of petroleum exploration// FRIDAID 1600679 https://hdl.handle.net/10037/13472 |
op_rights | openAccess |
publishDate | 2018 |
publisher | Nature Publishing Group |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/13472 2025-04-13T14:11:49+00:00 Novel biomineralization strategy in calcareous foraminifera Borrelli, Chiara Panieri, Giuliana Dahl, Trine Merete Neufeld, Kai 2018 https://hdl.handle.net/10037/13472 https://doi.org/10.1038/s41598-018-28400-2 eng eng Nature Publishing Group Scientific Reports info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ info:eu-repo/grantAgreement/RCN/PETROMAKS2/255150/Norway/Norwegian margin fluid systems and methane- derived carbonate crusts - Recent scientific advances in service of petroleum exploration// FRIDAID 1600679 https://hdl.handle.net/10037/13472 openAccess VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 Journal article Tidsskriftartikkel Peer reviewed 2018 ftunivtroemsoe https://doi.org/10.1038/s41598-018-28400-2 2025-03-14T05:17:56Z Source at https://doi.org/10.1038/s41598-018-28400-2 . Licensed CC BY-NC-ND 4.0. This work shows that calcareous benthic foraminifera are capable of agglutinating sedimentary particles also. In particular, we focus on Melonis barleeanus. Traditionally considered a calcareous species, our data revealed the presence of minute (~3 μm) sedimentary particles (silicate grains) inside the chamber walls of the examined shells. These particles were arranged in a definitive and systematic pattern, and the similar grain chemical characterization and size suggested a relatively high degree of selectivity in both modern and fossil specimens. Based on these results, we propose that M. barleeanus is capable of agglutinating sedimentary particles during the formation of a new chamber. The analysis of other calcareous foraminiferal species (e.g., Cassidulina neoteretis, Lobatula lobatula, Nonionella stella) did not reveal the presence of silicate grains in the shell of the specimens analyzed confirming this to be a characteristic of M. barleeanus. Considering that the isotopic and chemical composition of this species is widely used in paleoclimatic and paleoceanographic reconstructions, we used a mixing model to better constrain the influence of sedimentary particles on M. barleeanus δ 18 O data. Our model showed that the calcite δ 18 O would increase by ~0.9–2‰ if 10 wt% of feldspars (i.e., anorthite, albite, orthoclase) and quartz, respectively, were included in the analyzed shell. Based on these results, we emphasize that it is of paramount importance to consider M. barleeanus unusual biomineralization strategy during the interpretation of geological records and to investigate the presence of similar processes in other calcareous foraminiferal species. Article in Journal/Newspaper Arctic University of Tromsø: Munin Open Research Archive Stella ENVELOPE(-64.254,-64.254,-65.249,-65.249) Scientific Reports 8 1 |
spellingShingle | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 Borrelli, Chiara Panieri, Giuliana Dahl, Trine Merete Neufeld, Kai Novel biomineralization strategy in calcareous foraminifera |
title | Novel biomineralization strategy in calcareous foraminifera |
title_full | Novel biomineralization strategy in calcareous foraminifera |
title_fullStr | Novel biomineralization strategy in calcareous foraminifera |
title_full_unstemmed | Novel biomineralization strategy in calcareous foraminifera |
title_short | Novel biomineralization strategy in calcareous foraminifera |
title_sort | novel biomineralization strategy in calcareous foraminifera |
topic | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 |
topic_facet | VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 |
url | https://hdl.handle.net/10037/13472 https://doi.org/10.1038/s41598-018-28400-2 |