Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus

The lower Maastrichtian (Upper Cretaceous) section at Nahoryany, south of Lviv (western Ukraine), has been known as a rich source of fossils since 1843. However, the section is not available since a long time ago and fossils collected from it can only be studied in museum collections. In the present...

ver descrição completa

Detalhes bibliográficos
Autor principal: Marcin Machalski
Formato: Artigo
Idioma:English
Publicado em: Cambridge University Press 2024-01-01
coleção:Netherlands Journal of Geosciences
Assuntos:
Acesso em linha:https://www.cambridge.org/core/product/identifier/S0016774624000027/type/journal_article
_version_ 1827311460951261184
author Marcin Machalski
author_facet Marcin Machalski
author_sort Marcin Machalski
collection DOAJ
description The lower Maastrichtian (Upper Cretaceous) section at Nahoryany, south of Lviv (western Ukraine), has been known as a rich source of fossils since 1843. However, the section is not available since a long time ago and fossils collected from it can only be studied in museum collections. In the present paper, ammonites of the scaphitid genus Hoploscaphites are studied based on Nahoryany material, comprising Hoploscaphites pumilus, H. constrictus and H. sp. Specimens from Nahoryany in museum collections lack data on their provenance level within the section so it cannot be determined whether or not they occurred together or formed a succession; data on inoceramid bivalves indicate the presence of two successive zones at Nahoryany. Some specimens from Nahoryany here referred to as H. pumilus are similar to the controversial H. constrictus anterior from the lower Maastrichtian of Poland. This morphology suggests an ancestor–descendant relationship between H. pumilus and H. constrictus, a common species once considered as an informal index for the Boreal Maastrichtian in Europe. The inferred evolutionary transition from H. pumilus to H. constrictus was towards a less robust, recoiled shell, which would have enhanced the horizontal swimming ability and manoeuvrability of these cephalopods. Recoiling trends occurred in several lineages of Late Cretaceous scaphitids.
first_indexed 2024-04-24T20:19:20Z
format Article
id doaj.art-40a8cbb4843843beabef57c2bd33c2fb
institution Directory Open Access Journal
issn 0016-7746
1573-9708
language English
last_indexed 2024-04-24T20:19:20Z
publishDate 2024-01-01
publisher Cambridge University Press
record_format Article
series Netherlands Journal of Geosciences
spelling doaj.art-40a8cbb4843843beabef57c2bd33c2fb2024-03-22T08:49:21ZengCambridge University PressNetherlands Journal of Geosciences0016-77461573-97082024-01-0110310.1017/njg.2024.2Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictusMarcin Machalski0https://orcid.org/0000-0002-1121-4093Institute of Paleobiology, Polish Academy of Sciences, Warszawa, PolandThe lower Maastrichtian (Upper Cretaceous) section at Nahoryany, south of Lviv (western Ukraine), has been known as a rich source of fossils since 1843. However, the section is not available since a long time ago and fossils collected from it can only be studied in museum collections. In the present paper, ammonites of the scaphitid genus Hoploscaphites are studied based on Nahoryany material, comprising Hoploscaphites pumilus, H. constrictus and H. sp. Specimens from Nahoryany in museum collections lack data on their provenance level within the section so it cannot be determined whether or not they occurred together or formed a succession; data on inoceramid bivalves indicate the presence of two successive zones at Nahoryany. Some specimens from Nahoryany here referred to as H. pumilus are similar to the controversial H. constrictus anterior from the lower Maastrichtian of Poland. This morphology suggests an ancestor–descendant relationship between H. pumilus and H. constrictus, a common species once considered as an informal index for the Boreal Maastrichtian in Europe. The inferred evolutionary transition from H. pumilus to H. constrictus was towards a less robust, recoiled shell, which would have enhanced the horizontal swimming ability and manoeuvrability of these cephalopods. Recoiling trends occurred in several lineages of Late Cretaceous scaphitids.https://www.cambridge.org/core/product/identifier/S0016774624000027/type/journal_articleAmmonoideaCretaceousevolutionstratigraphy
spellingShingle Marcin Machalski
Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
Netherlands Journal of Geosciences
Ammonoidea
Cretaceous
evolution
stratigraphy
title Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
title_full Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
title_fullStr Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
title_full_unstemmed Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
title_short Scaphitid ammonites from the lower Maastrichtian of Nahoryany (western Ukraine) and discussion on the origin of Hoploscaphites constrictus
title_sort scaphitid ammonites from the lower maastrichtian of nahoryany western ukraine and discussion on the origin of hoploscaphites constrictus
topic Ammonoidea
Cretaceous
evolution
stratigraphy
url https://www.cambridge.org/core/product/identifier/S0016774624000027/type/journal_article
work_keys_str_mv AT marcinmachalski scaphitidammonitesfromthelowermaastrichtianofnahoryanywesternukraineanddiscussionontheoriginofhoploscaphitesconstrictus