New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids

The Triassic clam shrimp genus Aquilonoglypta Novojilov, 1958 was first erected based on a specimen collected from the Lower Triassic along the Laptev Sea coast of Russia. Its original diagnostic ornament was described as fish scale pits. Then, the genus was recovered in the Lower and Middle Triassi...

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Published in:Paleontological Research
Main Author: Li, Gang
Format: Report
Language:English
Published: PALAEONTOLOGICAL SOC JAPAN 2022
Subjects:
Online Access:http://ir.nigpas.ac.cn/handle/332004/40316
https://doi.org/10.2517/PR200028
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author Li, Gang
author_facet Li, Gang
author_sort Li, Gang
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
container_issue 1
container_title Paleontological Research
container_volume 26
description The Triassic clam shrimp genus Aquilonoglypta Novojilov, 1958 was first erected based on a specimen collected from the Lower Triassic along the Laptev Sea coast of Russia. Its original diagnostic ornament was described as fish scale pits. Then, the genus was recovered in the Lower and Middle Triassic in the Ordos Basin in northwestern China. Because the Chinese specimens have punctate ornamentation, they were interpreted as the ancestor of the Jurassic triglyptids. In this study the diagnosis of Aquilonoglypta is revised following a re-examination of the Russian type specimens under a scanning electron microscope (SEM). In Aquilonoglypta growth bands near the umbo are ornamented with polygonal fine reticulation, which transitions to puncta on growth bands in the middle part of the carapace. The ornamentation on growth bands in the ventral part of the carapace clearly shows the transition from the puncta to a size-increasing fine reticulation pattern. This research result shows that Aquilonoglypta could not be the close link with triglyptids because of lacking of the fine reticulation on growth bands in the dorsal part of the carapace in the latter. On the contrary Triglypta Wang, 1984 could be more closely related to Punctatestheria Zhang et al., 2017.
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Laptev Sea
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op_relation PALEONTOLOGICAL RESEARCH
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doi:10.2517/PR200028
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spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/40316 2025-04-06T14:57:56+00:00 New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids Li, Gang 2022 http://ir.nigpas.ac.cn/handle/332004/40316 https://doi.org/10.2517/PR200028 英语 eng PALAEONTOLOGICAL SOC JAPAN PALEONTOLOGICAL RESEARCH http://ir.nigpas.ac.cn/handle/332004/40316 doi:10.2517/PR200028 Aquilonoglypta clam shrimp Russia Spinicaudata taxonomy Triassic CRETACEOUS DALAZI FORMATION BIOSTRATIGRAPHIC SIGNIFICANCE BRANCHIOPODA SPINICAUDATA CONCHOSTRACAN FAUNA YIXIAN FORMATION BASIN REVISION CRUSTACEA PROVINCE AGE Paleontology 期刊论文 2022 ftchinacscnigpas https://doi.org/10.2517/PR200028 2025-03-10T08:37:33Z The Triassic clam shrimp genus Aquilonoglypta Novojilov, 1958 was first erected based on a specimen collected from the Lower Triassic along the Laptev Sea coast of Russia. Its original diagnostic ornament was described as fish scale pits. Then, the genus was recovered in the Lower and Middle Triassic in the Ordos Basin in northwestern China. Because the Chinese specimens have punctate ornamentation, they were interpreted as the ancestor of the Jurassic triglyptids. In this study the diagnosis of Aquilonoglypta is revised following a re-examination of the Russian type specimens under a scanning electron microscope (SEM). In Aquilonoglypta growth bands near the umbo are ornamented with polygonal fine reticulation, which transitions to puncta on growth bands in the middle part of the carapace. The ornamentation on growth bands in the ventral part of the carapace clearly shows the transition from the puncta to a size-increasing fine reticulation pattern. This research result shows that Aquilonoglypta could not be the close link with triglyptids because of lacking of the fine reticulation on growth bands in the dorsal part of the carapace in the latter. On the contrary Triglypta Wang, 1984 could be more closely related to Punctatestheria Zhang et al., 2017. Report laptev Laptev Sea Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Laptev Sea Paleontological Research 26 1
spellingShingle Aquilonoglypta
clam shrimp
Russia
Spinicaudata
taxonomy
Triassic
CRETACEOUS DALAZI FORMATION
BIOSTRATIGRAPHIC SIGNIFICANCE
BRANCHIOPODA SPINICAUDATA
CONCHOSTRACAN FAUNA
YIXIAN FORMATION
BASIN
REVISION
CRUSTACEA
PROVINCE
AGE
Paleontology
Li, Gang
New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title_full New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title_fullStr New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title_full_unstemmed New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title_short New taxonomic features of fossil clam shrimp Aquilonoglypta (Spinicaudata) and its implication for origin of triglyptids
title_sort new taxonomic features of fossil clam shrimp aquilonoglypta (spinicaudata) and its implication for origin of triglyptids
topic Aquilonoglypta
clam shrimp
Russia
Spinicaudata
taxonomy
Triassic
CRETACEOUS DALAZI FORMATION
BIOSTRATIGRAPHIC SIGNIFICANCE
BRANCHIOPODA SPINICAUDATA
CONCHOSTRACAN FAUNA
YIXIAN FORMATION
BASIN
REVISION
CRUSTACEA
PROVINCE
AGE
Paleontology
topic_facet Aquilonoglypta
clam shrimp
Russia
Spinicaudata
taxonomy
Triassic
CRETACEOUS DALAZI FORMATION
BIOSTRATIGRAPHIC SIGNIFICANCE
BRANCHIOPODA SPINICAUDATA
CONCHOSTRACAN FAUNA
YIXIAN FORMATION
BASIN
REVISION
CRUSTACEA
PROVINCE
AGE
Paleontology
url http://ir.nigpas.ac.cn/handle/332004/40316
https://doi.org/10.2517/PR200028