Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights

The morphology of the adaxial structures of cones belonging to Palissya Endlicher 1847 emend. nov. are reinterpreted based on exquisitely preserved permineralised material from the Lower Cretaceous of Queensland. Although the material was not found in situ, it likely derives from the Orallo Formatio...

Full description

Bibliographic Details
Main Authors: Gary A Pattemore, Andrew Rozefelds
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10779/cqu.20445678.v1
id ftcquniportalfig:oai:figshare.com:article/20445678
record_format openpolar
spelling ftcquniportalfig:oai:figshare.com:article/20445678 2023-05-15T13:47:34+02:00 Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights Gary A Pattemore Andrew Rozefelds 2019-12-16T00:00:00Z http://hdl.handle.net/10779/cqu.20445678.v1 unknown https://figshare.com/articles/journal_contribution/Palissya_-_Absolutely_incomprehensible_or_surprisingly_interpretable_A_new_morphological_model_affiliations_and_phylogenetic_insights/20445678 http://hdl.handle.net/10779/cqu.20445678.v1 CC BY-NC-ND 3.0 CC-BY-NC-ND Palaeontology (incl. Palynology) Knezourocarpon Lower cretaceous Orallo formation Palissya Queensland Surat Basin Valanginian Paleontology Text Journal contribution 2019 ftcquniportalfig 2022-09-13T10:05:27Z The morphology of the adaxial structures of cones belonging to Palissya Endlicher 1847 emend. nov. are reinterpreted based on exquisitely preserved permineralised material from the Lower Cretaceous of Queensland. Although the material was not found in situ, it likely derives from the Orallo Formation, which is Valanginian in age. The cones have dual vascular bundles in each bract/scale complex, and the different tissue types in the bract and ovule/scale complex support interpretation of the cone as a compound structure. Since the early twentieth century it has been widely accepted that each ovule is surrounded by a cup-shaped structure, but the detailed morphology of the "cup" has hitherto been unclear. These new three-dimensionally preserved specimens with in situ ovules are described as Palissya tillackiorum sp. nov. This study demonstrates that the "cup" is formed from a pair of thin scales that subtend but are not fused to each ovule; each pair of scales comprises a thicker outer and thinner inner scale. The organographic relationships among ovules and scales in Palissya show a high degree of synorganisation. The adaxial surface of the bract/scale complex has 2-6 pairs of erect (orthotropous) ovules. The ovule/scale units are arranged symmetrically in two parallel rows on either side of the midline of the bract/scale. Individual ovule/scale units are comparable to those seen in extant Podocarpaceae and Taxaceae. The ovules are thin-walled and are interpreted to have a single integument and a non-thickened (non-lignified) micropyle. These new insights allow reinterpretation of material previously referred to Palissya. A new species is described from Yorkshire, England, as P. harrisii C.R. Hill ex Pattemore & Rozefelds sp. nov. All species based on well preserved cones are reconsidered herein: P. sphenolepis (Braun 1843) Nathorst 1908 emend. Florin 1958, P. elegans Parris, Drinnan & Cantrill 1995 emend. nov., P. bartrumii Edwards 1934 emend. nov., P. antarctica Cantrill 2000 and P. hunanensis Wang ... Other Non-Article Part of Journal/Newspaper Antarc* Antarctica CQUniversity: acquire Parris ENVELOPE(9.789,9.789,62.915,62.915) Queensland The Cones ENVELOPE(78.344,78.344,-68.635,-68.635)
institution Open Polar
collection CQUniversity: acquire
op_collection_id ftcquniportalfig
language unknown
topic Palaeontology (incl. Palynology)
Knezourocarpon
Lower cretaceous
Orallo formation
Palissya
Queensland
Surat Basin
Valanginian
Paleontology
spellingShingle Palaeontology (incl. Palynology)
Knezourocarpon
Lower cretaceous
Orallo formation
Palissya
Queensland
Surat Basin
Valanginian
Paleontology
Gary A Pattemore
Andrew Rozefelds
Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
topic_facet Palaeontology (incl. Palynology)
Knezourocarpon
Lower cretaceous
Orallo formation
Palissya
Queensland
Surat Basin
Valanginian
Paleontology
description The morphology of the adaxial structures of cones belonging to Palissya Endlicher 1847 emend. nov. are reinterpreted based on exquisitely preserved permineralised material from the Lower Cretaceous of Queensland. Although the material was not found in situ, it likely derives from the Orallo Formation, which is Valanginian in age. The cones have dual vascular bundles in each bract/scale complex, and the different tissue types in the bract and ovule/scale complex support interpretation of the cone as a compound structure. Since the early twentieth century it has been widely accepted that each ovule is surrounded by a cup-shaped structure, but the detailed morphology of the "cup" has hitherto been unclear. These new three-dimensionally preserved specimens with in situ ovules are described as Palissya tillackiorum sp. nov. This study demonstrates that the "cup" is formed from a pair of thin scales that subtend but are not fused to each ovule; each pair of scales comprises a thicker outer and thinner inner scale. The organographic relationships among ovules and scales in Palissya show a high degree of synorganisation. The adaxial surface of the bract/scale complex has 2-6 pairs of erect (orthotropous) ovules. The ovule/scale units are arranged symmetrically in two parallel rows on either side of the midline of the bract/scale. Individual ovule/scale units are comparable to those seen in extant Podocarpaceae and Taxaceae. The ovules are thin-walled and are interpreted to have a single integument and a non-thickened (non-lignified) micropyle. These new insights allow reinterpretation of material previously referred to Palissya. A new species is described from Yorkshire, England, as P. harrisii C.R. Hill ex Pattemore & Rozefelds sp. nov. All species based on well preserved cones are reconsidered herein: P. sphenolepis (Braun 1843) Nathorst 1908 emend. Florin 1958, P. elegans Parris, Drinnan & Cantrill 1995 emend. nov., P. bartrumii Edwards 1934 emend. nov., P. antarctica Cantrill 2000 and P. hunanensis Wang ...
format Other Non-Article Part of Journal/Newspaper
author Gary A Pattemore
Andrew Rozefelds
author_facet Gary A Pattemore
Andrew Rozefelds
author_sort Gary A Pattemore
title Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
title_short Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
title_full Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
title_fullStr Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
title_full_unstemmed Palissya - Absolutely incomprehensible or surprisingly interpretable: A new morphological model, affiliations and phylogenetic insights
title_sort palissya - absolutely incomprehensible or surprisingly interpretable: a new morphological model, affiliations and phylogenetic insights
publishDate 2019
url http://hdl.handle.net/10779/cqu.20445678.v1
long_lat ENVELOPE(9.789,9.789,62.915,62.915)
ENVELOPE(78.344,78.344,-68.635,-68.635)
geographic Parris
Queensland
The Cones
geographic_facet Parris
Queensland
The Cones
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://figshare.com/articles/journal_contribution/Palissya_-_Absolutely_incomprehensible_or_surprisingly_interpretable_A_new_morphological_model_affiliations_and_phylogenetic_insights/20445678
http://hdl.handle.net/10779/cqu.20445678.v1
op_rights CC BY-NC-ND 3.0
op_rightsnorm CC-BY-NC-ND
_version_ 1766247309433110528