Spore Evidence for the Origin of Isoetalean Lycopsids?

A new hypothesis about the origin of isoetalean lycopsids was proposed based on palynological data. The occurrence of three apical papillae on the proximal surfaces of miospores is a significant palynological feature that is clearly defined in both isoetalean and selaginellalean clades. Three apical...

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Main Authors: Jiří Bek, Jana Votočková Frojdová
Format: Article
Language:English
Published: MDPI AG 2023-07-01
Series:Life
Subjects:
Online Access:https://www.mdpi.com/2075-1729/13/7/1546
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author Jiří Bek
Jana Votočková Frojdová
author_facet Jiří Bek
Jana Votočková Frojdová
author_sort Jiří Bek
collection DOAJ
description A new hypothesis about the origin of isoetalean lycopsids was proposed based on palynological data. The occurrence of three apical papillae on the proximal surfaces of miospores is a significant palynological feature that is clearly defined in both isoetalean and selaginellalean clades. Three apical papillae appeared for the first time within lower Silurian (Wenlockian ca. 430 My) and only in rhyniophytoid plants. Using this observation, we suggest that isoetalean lycopsids could have evolved directly from rhyniophytoids and not from protolepidodendralean lycopsids in the middle Devonian (Eifelian–Givetian) as previously suggested, because protolepidodendralean spores do not possess three apical papillae. Spores with three apical papillae, reported as dispersed as well as in situ, were recorded continuously from the lower Silurian (Wenlockian) through the Devonian, Carboniferous, Permian, Mesozoic to Cenozoic era and form a phylogenetically independent lineage.
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spelling doaj.art-d41f17b6b030411f811e2e23e01257bd2023-11-18T20:10:00ZengMDPI AGLife2075-17292023-07-01137154610.3390/life13071546Spore Evidence for the Origin of Isoetalean Lycopsids?Jiří Bek0Jana Votočková Frojdová1Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 269, 16500 Prague, Czech RepublicInstitute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 269, 16500 Prague, Czech RepublicA new hypothesis about the origin of isoetalean lycopsids was proposed based on palynological data. The occurrence of three apical papillae on the proximal surfaces of miospores is a significant palynological feature that is clearly defined in both isoetalean and selaginellalean clades. Three apical papillae appeared for the first time within lower Silurian (Wenlockian ca. 430 My) and only in rhyniophytoid plants. Using this observation, we suggest that isoetalean lycopsids could have evolved directly from rhyniophytoids and not from protolepidodendralean lycopsids in the middle Devonian (Eifelian–Givetian) as previously suggested, because protolepidodendralean spores do not possess three apical papillae. Spores with three apical papillae, reported as dispersed as well as in situ, were recorded continuously from the lower Silurian (Wenlockian) through the Devonian, Carboniferous, Permian, Mesozoic to Cenozoic era and form a phylogenetically independent lineage.https://www.mdpi.com/2075-1729/13/7/1546lycopsidsisoetaleansselaginellaleansrhyniophytessporespalynology
spellingShingle Jiří Bek
Jana Votočková Frojdová
Spore Evidence for the Origin of Isoetalean Lycopsids?
Life
lycopsids
isoetaleans
selaginellaleans
rhyniophytes
spores
palynology
title Spore Evidence for the Origin of Isoetalean Lycopsids?
title_full Spore Evidence for the Origin of Isoetalean Lycopsids?
title_fullStr Spore Evidence for the Origin of Isoetalean Lycopsids?
title_full_unstemmed Spore Evidence for the Origin of Isoetalean Lycopsids?
title_short Spore Evidence for the Origin of Isoetalean Lycopsids?
title_sort spore evidence for the origin of isoetalean lycopsids
topic lycopsids
isoetaleans
selaginellaleans
rhyniophytes
spores
palynology
url https://www.mdpi.com/2075-1729/13/7/1546
work_keys_str_mv AT jiribek sporeevidencefortheoriginofisoetaleanlycopsids
AT janavotockovafrojdova sporeevidencefortheoriginofisoetaleanlycopsids