Does dinocyst wall composition really reflect trophic affinity? New evidence from ATR micro-FTIR spectroscopy measurements.

attenuated total reflection micro-Fourier transform infrared spectroscopy bleaching dinosporin composition optical photothermal infrared spectroscopy organic-walled dinocysts pigments spectrochemical methods sunscreen synchrotron radiation trophic affinity

Journal

Journal of phycology
ISSN: 1529-8817
Titre abrégé: J Phycol
Pays: United States
ID NLM: 9882935

Informations de publication

Date de publication:
Oct 2023
Historique:
revised: 02 05 2023
received: 22 12 2022
accepted: 21 07 2023
pubmed: 25 8 2023
medline: 25 8 2023
entrez: 25 8 2023
Statut: ppublish

Résumé

Attenuated total reflection (ATR) microscope Fourier transform infrared (micro-FTIR) spectroscopy was used to investigate the dinosporin composition in the walls of modern, organic-walled dinoflagellate resting cysts (dinocysts). Variable cyst wall compositions were observed, which led to the erection of four spectrochemical groups, some with striking similarities to other resistant biomacromolecules such as sporopollenin and algaenan. Furthermore, possible proxies derivable from the spectrochemical composition of modern and fossil dinocysts were discussed. The color of the dinocyst walls was reflected in the spectral data. When comparing that color with a standard and the results of a series of bleaching experiments with oxidative agents, eumelanin was assigned as a likely pigment contributing to the observed color. Following this assignment, the role of eumelanin as an ultraviolet sunscreen in colored dinocysts was hypothesized, and its implications on the autofluorescence and morphological preservation of dinocysts were further discussed. Unlike what had previously been assumed, it was shown that micro-FTIR data from dinocysts cannot be used to unambiguously infer trophic affinities of their associated cells. Finally, using methods with high spatial resolutions (synchrotron transmission micro-FTIR and optical photothermal infrared spectroscopy), it was shown that dinocyst wall layers are chemically homogenous at the probed scales. This study fills a large knowledge gap in our understanding of the chemical nature of dinocyst walls and has nuanced certain assumptions and interpretations made in the past.

Identifiants

pubmed: 37623312
doi: 10.1111/jpy.13382
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

1064-1084

Subventions

Organisme : Fonds Wetenschappelijk Onderzoek
ID : K210522N
Organisme : Herculesstichting
ID : FT-IMAGER Project-AUGE/13/16

Informations de copyright

© 2023 Phycological Society of America.

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Auteurs

Pjotr Meyvisch (P)

Department of Geology, Ghent University, Ghent, Belgium.

Pieter Roger Gurdebeke (PR)

Department of Geology, Ghent University, Ghent, Belgium.

Christophe Sandt (C)

SMIS Beamline, SOLEIL Synchrotron, Paris, France.

Vera Pospelova (V)

Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, Minnesota, USA.

Henk Vrielinck (H)

Department of Solid-State Sciences, Ghent University, Ghent, Belgium.

Ferenc Borondics (F)

SMIS Beamline, SOLEIL Synchrotron, Paris, France.

Stephen Louwye (S)

Department of Geology, Ghent University, Ghent, Belgium.

Classifications MeSH