Data from: Enigmatic Multiplicisphaeridium-type acritarch from the Pleistocene of Marmara Sea: morphological and spectroscopic evidence for a chytrid-like new taxon
Data files
May 22, 2026 version files 826.61 KB
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Data_1.csv
824.56 KB
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README.md
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Abstract
An enigmatic, yellowish-brown, variably branched organic-walled microfossil (palynomorph) marks the Late Glacial Maximum of Upper Pleistocene sediments in the Marmara Sea. This taxon, previously called a Multiplicisphaeridium-type acritarch, a putative algal cyst, or a possible chytrid fungus, virtually disappears at the end of the Ponto-Caspian lacustrine phase, making it a valuable marker for regional ecostratigraphic correlation. However, uncertainty surrounding its biological affinity limits interpretations of its taxonomy, palaeoecology, evolutionary history, and broader geographic significance. We document the morphology and variability of well-preserved cf. Multiplicisphaeridium specimens from Marmara and Black Sea sediment cores using interference light microscopy and scanning electron microscopy. Detailed morphological comparisons with visually similar acritarchs, chytrids, and dinoflagellates indicate a plausible, though non-definitive, affinity with chytrid fungi and exclude pre-Quaternary sedimentary reworking. Compositional analyses using attenuated total reflection Fourier transform infrared microspectroscopy reveal a close biomacromolecular match between cf. Multiplicisphaeridium and co-occurring chytrid sporangia, including evidence of wall melanisation potentially characteristic of chytrids but distinct from other fungal clades. Additional comparative analyses of sporangia from extant marine Rhizophydium further contextualize chytrid wall taphonomy. The combined morphological and molecular evidence favours a chytrid-like affinity and demonstrates distinction from true Multiplicisphaeridium acritarchs, but does not justify assignment to a known chytrid lineage (extant Arkaya is identified as a potential close analogue). We therefore erect a new genus and species within the Acritarcha, Palaeoarkaya similis gen. et sp. nov., and discuss its potential significance in low-salinity glacial palaeoenvironments. This integrative morpho-molecular approach confirms earlier evidence of possible fungal affinity among acritarchs.
Dataset DOI: 10.5061/dryad.hdr7sqw06
Description of the data and file structure
File: Data_1.csv
Description: The dataset includes all ATR µ-FTIR spectra used in the associated manuscript. Apart from atmospheric compensation (= removal of water vapour and carbon dioxide bands), the spectra have not been processed. The dataset is formatted to be directly importable into the "File" widget of the open-source Quasar software (https://quasar.codes/) used in the manuscript. Numerical features and categorical metavariables should be read in correctly.
The first row of the dataset contains the column headers; the second and third rows contain labels that ensure a correct read-in of the numerical features and categorical metavariables into Quasar.
In the first row, numerical column headers (605.52712–4493.24264) represent wavenumber values (x-axis of ATR µ-FTIR spectra; unit = 1/cm); row values in these columns represent corresponding absorbance values (y-axis; unit = arbitrary units). From the fourth row and down, each row represents one spectrum with associated metadata (Spectrum name, Taxon, Organism group, Observed color, Biomacromolecular components, Sample, Age, Acid processing).
Applied data processing is extensively described in the Materials and Methods section of the manuscript.
Variables
- Categorical variables: Spectrum name, Taxon, Organism group, Observed color, Biomacromolecular components, Sample, Age, Acid processing (colums 1–8).
- Numerical features: Wavenumber values from 605.52712–4493.24264 (remaining 2017 columns) with associated Absorbance values as row values.
Code/software
Open-source Quasar software (https://quasar.codes/)
Compatible with all major operating systems
Access information
N/A
