Changes in the microbial community associated with the large benthic foraminifera cycloclypeus carpenteri, along a depth gradient
| Authors |
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|---|---|
| Publication date | 01-2024 |
| Journal | Journal of Foraminiferal Research |
| Volume | Issue number | 54 | 1 |
| Pages (from-to) | 65-74 |
| Number of pages | 10 |
| Organisations |
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| Abstract |
Cycloclypeus carpenteri is one of the deepest living large benthic
foraminifera. It has an obligatory relationship with diatom
photosymbionts, and, in addition, houses a diverse prokaryotic
community. Variations in the eukaryotic and prokaryotic endobiotic
community composition might be key in allowing Cycloclypeus to occur in low light environments. We assessed the variability of the prokaryotic and eukaryotic communities associated with Cycloclypeus
along a depth gradient from 50 to 130 m at two locations in the
Federated States of Micronesia (Northwest Pacific) by metabarcoding of
the 18S V9 rRNA region for eukaryotes and the 16S V3-V4 rRNA region for
prokaryotes. We observed a single foraminiferal operational taxonomic
unit (OTU), as well as a single dominant diatom OTU that was abundant in
all sequenced specimens. Both the prokaryotic and the eukaryotic
endobiotic communities (excluding the dominant diatom) changed with
water depth and associated irradiance levels. We observed a distinct
change in the prokaryotic community composition around 90–100 m water
depth at Pohnpei, equivalent to ∼1% surface radiation. This change in
microbial communities in the Cycloclypeus holobiont suggests a
potential role of the associated microbial communities in accommodating
differences in (micro)habitat, although we cannot exclude that the
prokaryote community is to a large extent driven by their community
composition in the ambient environment.
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| Document type | Article |
| Note | With supplementary material. |
| Language | English |
| Published at | https://doi.org/10.2113/gsjfr.54.1.65 |
| Other links | https://www.scopus.com/pages/publications/85188785710 |
| Downloads |
i1943-264x-54-1-65
(Final published version)
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| Supplementary materials | |
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