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  • 494-2; 496-2; 511-2; 512-1; 513-2; 528-2; 530-1; 532-2; 536-1; 538-1; Center for Marine Environmental Sciences; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DNA concentration; Elevation of event; Event label; Flemish Cap; Foraminifera; Foraminifera, planktic, number of reads; GC; GeoB18515-2; GeoB18517-2; GeoB18532-2; GeoB18533-1; GeoB18534-2; GeoB18549-2; GeoB18551-1; GeoB18553-2; GeoB18557-1; GeoB18559-1; Globothalamea, number of reads; Gravity corer; Latitude of event; Location of event; Longitude of event; Maria S. Merian; MARUM; Metabarcoding; microfossils; Monothalamea, number of reads; MSM39; MUC; MultiCorer; North Atlantic; Operational taxonomic unit; Orphan Basin; Orphan Knoll; Ratio; Reads; Sample code/label; sedimentary ancient DNA; SE Grand Banks Slope; SW Grand Banks Slope; Tubothalamea, number of reads  (1)
  • Center for Marine Environmental Sciences; Foraminifera; MARUM; Metabarcoding; microfossils; North Atlantic; sedimentary ancient DNA  (1)
  • Intertidal  (1)
  • Biodiversity
  • 2020-2024  (3)
Document type
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  • 1
    Publication Date: 2024-02-14
    Description: Environmental DNA (eDNA) metabarcoding of marine sediments has revealed large amounts of sequences assigned to planktonic taxa. How this planktonic eDNA is delivered on the seafloor and preserved in the sediment is not well understood. We address these questions by comparing metabarcoding and microfossil foraminifera assemblages in sediment cores taken off Newfoundland across a strong ecological gradient. We detected planktonic foraminifera eDNA down to 30 cm and observed that the planktonic/benthic amplicon ratio changed with depth. The relative proportion of planktonic foraminiferal amplicons remained low from the surface down to 10 cm, likely due to the presence of DNA from living benthic foraminifera. Below 10 cm, the relative proportion of planktonic foraminifera amplicons rocketed, likely reflecting the higher proportion of planktonic eDNA in the DNA burial flux. In addition, the microfossil and metabarcoding assemblages showed a congruent pattern indicating that planktonic foraminifera eDNA is deposited without substantial lateral advection and preserves regional biogeographical patterns, indicating deposition by a similar mechanism as the foraminiferal shells. Our study shows that the planktonic eDNA preserved in marine sediments has the potential to record climatic and biotic changes in the pelagic community with the same spatial and temporal resolution as microfossils.
    Keywords: Center for Marine Environmental Sciences; Foraminifera; MARUM; Metabarcoding; microfossils; North Atlantic; sedimentary ancient DNA
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-14
    Keywords: 494-2; 496-2; 511-2; 512-1; 513-2; 528-2; 530-1; 532-2; 536-1; 538-1; Center for Marine Environmental Sciences; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DNA concentration; Elevation of event; Event label; Flemish Cap; Foraminifera; Foraminifera, planktic, number of reads; GC; GeoB18515-2; GeoB18517-2; GeoB18532-2; GeoB18533-1; GeoB18534-2; GeoB18549-2; GeoB18551-1; GeoB18553-2; GeoB18557-1; GeoB18559-1; Globothalamea, number of reads; Gravity corer; Latitude of event; Location of event; Longitude of event; Maria S. Merian; MARUM; Metabarcoding; microfossils; Monothalamea, number of reads; MSM39; MUC; MultiCorer; North Atlantic; Operational taxonomic unit; Orphan Basin; Orphan Knoll; Ratio; Reads; Sample code/label; sedimentary ancient DNA; SE Grand Banks Slope; SW Grand Banks Slope; Tubothalamea, number of reads
    Type: Dataset
    Format: text/tab-separated-values, 1993 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-05-30
    Description: Foraminifera are a species-rich phylum of rhizarian protists that are highly abundant in most marine environments. Molecular methods such as metabarcoding have revealed a high, yet undescribed diversity of Foraminifera. However, so far only one molecular marker, the 18S ribosomal RNA, was available for metabarcoding studies on Foraminifera. Primers that allow amplification of foraminiferal mitochondrial cytochrome oxidase I (COI) and identification of Foraminifera species were recently published. Here we test the performance of these primers for the amplification of whole foraminiferal communities, and compare their performance to that of the highly degenerate LerayXT primers, which amplify the same COI region in a wide range of eukaryotes. We applied metabarcoding to 48 samples taken along three transects spanning a North Sea beach in the Netherlands from dunes to the low tide level, and analysed both sediment samples and meiofauna samples, which contained taxa between 42 mm and 1 mm in body size obtained by decantation from sand samples. We used single-cell metabarcoding (Girard et al., 2022) to generate a COI reference library containing 32 species of Foraminifera, and used this to taxonomically annotate our community metabarcoding data. Our analyses show that the highly degenerate LerayXT primers do not amplify Foraminifera, while the Foraminifera primers are highly Foraminifera- specific, with about 90% of reads assigned to Foraminifera and amplifying taxa from all major groups, i.e., monothalamids, Globothalamea, and Tubothalamea. We identified 176 Foraminifera ASVs and found a change in Foraminifera community composition along the beach transects from high tide to low tide level, and a dominance of single-chambered monothalamid Foraminifera. Our results highlight that COI metabarcoding can be a powerful tool for assessing Foraminiferal communities.
    Keywords: Foraminifera ; Metabarcoding ; Beach ; Community composition ; Intertidal ; Molecular ; biodiversity
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Limitation Availability
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