Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China
Acrotretoids, one of the oldest brachiopod groups, are abundant in the Lower Cambrian Jiulaodong Formation. The shell of Linnarssonia sp. is composed of two layers: a primary layer and a columnar secondary layer. The primary layer is mostly exfoliated, resulting in exposure of the openings to the ce...
Published in: | Lethaia |
---|---|
Main Authors: | , |
Format: | Report |
Language: | English |
Published: |
WILEY-BLACKWELL
2004
|
Subjects: | |
Online Access: | http://ir.nigpas.ac.cn/handle/332004/1036 https://doi.org/10.1080/00241160410006528 |
_version_ | 1828691730213371904 |
---|---|
author | Feng, WM (冯伟民) Kobayashi, I |
author_facet | Feng, WM (冯伟民) Kobayashi, I |
author_sort | Feng, WM (冯伟民) |
collection | Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) |
container_issue | 3 |
container_start_page | 263 |
container_title | Lethaia |
container_volume | 37 |
description | Acrotretoids, one of the oldest brachiopod groups, are abundant in the Lower Cambrian Jiulaodong Formation. The shell of Linnarssonia sp. is composed of two layers: a primary layer and a columnar secondary layer. The primary layer is mostly exfoliated, resulting in exposure of the openings to the central canal of the columns. Filae are seen on the surface of the columnar layer, indicating that the columnar secondary layer has influenced changes in ornament on the shell surface. The larval shell has only very weak ripples; the post-larval shell has obvious concentric ribs. Small pits of variable shape cover almost the entire shell surface. The secondary layer is composed of several columnar laminations, each of which comprises both the upper and lower laminae and the cylindrical columns between them. On the inner side of shell the thin columnar laminations increase. The new microstructural data show that two shell layers are developed in Early Cambrian acrotretoid brachiopods; the columnar lamination may be a primitive feature of the microstructural development of the Brachiopoda and may help establish the affinity between different stem-group brachiopods. |
format | Report |
genre | Greenland |
genre_facet | Greenland |
geographic | Greenland |
geographic_facet | Greenland |
id | ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/1036 |
institution | Open Polar |
language | English |
op_collection_id | ftchinacscnigpas |
op_container_end_page | 270 |
op_doi | https://doi.org/10.1080/00241160410006528 |
op_relation | LETHAIA http://ir.nigpas.ac.cn/handle/332004/1036 doi:10.1080/00241160410006528 |
publishDate | 2004 |
publisher | WILEY-BLACKWELL |
record_format | openpolar |
spelling | ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/1036 2025-04-06T14:54:08+00:00 Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China Feng, WM (冯伟民) Kobayashi, I 2004-09-01 http://ir.nigpas.ac.cn/handle/332004/1036 https://doi.org/10.1080/00241160410006528 英语 eng WILEY-BLACKWELL LETHAIA http://ir.nigpas.ac.cn/handle/332004/1036 doi:10.1080/00241160410006528 Acrotretoids Early Cambrian Jiulaodong Formation Linnarssonia Microstructure Sichuan Stem Group Brachiopod Shell Structure Acrotretida Greenland Evolution Micrina Paleontology 期刊论文 2004 ftchinacscnigpas https://doi.org/10.1080/00241160410006528 2025-03-10T08:37:33Z Acrotretoids, one of the oldest brachiopod groups, are abundant in the Lower Cambrian Jiulaodong Formation. The shell of Linnarssonia sp. is composed of two layers: a primary layer and a columnar secondary layer. The primary layer is mostly exfoliated, resulting in exposure of the openings to the central canal of the columns. Filae are seen on the surface of the columnar layer, indicating that the columnar secondary layer has influenced changes in ornament on the shell surface. The larval shell has only very weak ripples; the post-larval shell has obvious concentric ribs. Small pits of variable shape cover almost the entire shell surface. The secondary layer is composed of several columnar laminations, each of which comprises both the upper and lower laminae and the cylindrical columns between them. On the inner side of shell the thin columnar laminations increase. The new microstructural data show that two shell layers are developed in Early Cambrian acrotretoid brachiopods; the columnar lamination may be a primitive feature of the microstructural development of the Brachiopoda and may help establish the affinity between different stem-group brachiopods. Report Greenland Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Greenland Lethaia 37 3 263 270 |
spellingShingle | Acrotretoids Early Cambrian Jiulaodong Formation Linnarssonia Microstructure Sichuan Stem Group Brachiopod Shell Structure Acrotretida Greenland Evolution Micrina Paleontology Feng, WM (冯伟民) Kobayashi, I Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title | Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title_full | Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title_fullStr | Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title_full_unstemmed | Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title_short | Microstructure of the linguliformean brachiopod Linnarssonia from the Lower Cambrian of Sichuan, China |
title_sort | microstructure of the linguliformean brachiopod linnarssonia from the lower cambrian of sichuan, china |
topic | Acrotretoids Early Cambrian Jiulaodong Formation Linnarssonia Microstructure Sichuan Stem Group Brachiopod Shell Structure Acrotretida Greenland Evolution Micrina Paleontology |
topic_facet | Acrotretoids Early Cambrian Jiulaodong Formation Linnarssonia Microstructure Sichuan Stem Group Brachiopod Shell Structure Acrotretida Greenland Evolution Micrina Paleontology |
url | http://ir.nigpas.ac.cn/handle/332004/1036 https://doi.org/10.1080/00241160410006528 |