Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

View through Europeana Collections
Linguliform brachiopods were important components of early Cambrian benthic communities. However, exceptionally preserved soft parts in Cambrian linguliform brachiopods are extremely sparse, and the most important findings are from the early Cambrian Chengjiang Konservat Lagerstatte of Kunming, southern China. Here we describe the first record of preserved soft-part anatomy in a linguli form brachiopod from the early Cambrian Guanshan fauna (Wu longging Formation, Palaeolenus Zone); a unit which is considerably younger than the Chengjiang fauna. The well preserved soft anatomy include linguliform pedicles, marginal setae and, in a few cases, an intact lophophore imprint. The pedicle has pronounced surface annulations, with its proximal-most part enclosing the apex of the ventral pseudointerarea; the pedicle is up to 51 mm long, corresponding to more than 4 times the sagittal length of the shell, and 12% of the maximum valve width. In details of their preservation, these new fossils exhibit striking similarities with the linguliforms from the older Chengjiang fauna, and all specimens are preserved in a compressed state as flattened impressions. The new linguliform has an elongate oval to subtriangular shell and an elongate triangular ventral pseudointerarea; the pedicle emerged from an apical foramen through a poorly preserved internal pedicle tube. The new linguliform is most similar to the mostly organic-shelled siphonotretoid-like brachiopod Acanthotretella spinosa, recently described from the classic middle Cambrian Burgess Shale Konservat Lagerstatte, British Columbia, Canada. The new species Acanthotretella decaius sp. nov. is described; it differs from A. spinosa in having a slightly thicker pedicle, and a larger and more rigid, probably partly mineralised shell, indicating that the mostly organic shell of A. spinosa may represent a secondary reduction of shell mineralisation. However, the spine-like setae of the new species are unfortunately poorly preserved only at the margin of the shell, but the new species is referred tentatively to the Superfamily Siphonotretoidea. The occurrence of A. decaius in the Guanshan fauna is the first lower Cambrian (Series 2, early Stage 4) record of both Acanthotretella and siphonotretoids, and it represents the first description of a lophophore and digestive tract from the siphonotretoid lineage.
image-zoom
Title: Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China
Description:
Linguliform brachiopods were important components of early Cambrian benthic communities.
However, exceptionally preserved soft parts in Cambrian linguliform brachiopods are extremely sparse, and the most important findings are from the early Cambrian Chengjiang Konservat Lagerstatte of Kunming, southern China.
Here we describe the first record of preserved soft-part anatomy in a linguli form brachiopod from the early Cambrian Guanshan fauna (Wu longging Formation, Palaeolenus Zone); a unit which is considerably younger than the Chengjiang fauna.
The well preserved soft anatomy include linguliform pedicles, marginal setae and, in a few cases, an intact lophophore imprint.
The pedicle has pronounced surface annulations, with its proximal-most part enclosing the apex of the ventral pseudointerarea; the pedicle is up to 51 mm long, corresponding to more than 4 times the sagittal length of the shell, and 12% of the maximum valve width.
In details of their preservation, these new fossils exhibit striking similarities with the linguliforms from the older Chengjiang fauna, and all specimens are preserved in a compressed state as flattened impressions.
The new linguliform has an elongate oval to subtriangular shell and an elongate triangular ventral pseudointerarea; the pedicle emerged from an apical foramen through a poorly preserved internal pedicle tube.
The new linguliform is most similar to the mostly organic-shelled siphonotretoid-like brachiopod Acanthotretella spinosa, recently described from the classic middle Cambrian Burgess Shale Konservat Lagerstatte, British Columbia, Canada.
The new species Acanthotretella decaius sp.
nov.
is described; it differs from A.
spinosa in having a slightly thicker pedicle, and a larger and more rigid, probably partly mineralised shell, indicating that the mostly organic shell of A.
spinosa may represent a secondary reduction of shell mineralisation.
However, the spine-like setae of the new species are unfortunately poorly preserved only at the margin of the shell, but the new species is referred tentatively to the Superfamily Siphonotretoidea.
The occurrence of A.
decaius in the Guanshan fauna is the first lower Cambrian (Series 2, early Stage 4) record of both Acanthotretella and siphonotretoids, and it represents the first description of a lophophore and digestive tract from the siphonotretoid lineage.

Related Results

Cambrian
Cambrian
The initial Cambrian record in most of the project area consists of medial BonniaðOlenellus Zone and younger Lower Cambrian strata overlying a Precambrian surface of various ages. ...
New Vetulicoliids from the Lower Cambrian Guanshan Fauna, Kunming
New Vetulicoliids from the Lower Cambrian Guanshan Fauna, Kunming
Abstract  The Guanshan Fauna, a soft‐bodied fauna intermediate between the Chengjiang Fauna and the Kaili Fauna and also the Burgess Shale Fauna stratigraphically, consists of tril...
β‐diversity fluctuations in Early–Mid Ordovician brachiopod communities of South China
β‐diversity fluctuations in Early–Mid Ordovician brachiopod communities of South China
AbstractLower to Middle Ordovician transitional strata (Acrograptus filiformis Biozone to Exigraptus clavus Biozone) of the Upper Yangtze Platform contain rich and diverse brachiop...
Tectonic evolution of an Early Cambrian foreland basin in the northwest Yangtze Block, South China
Tectonic evolution of an Early Cambrian foreland basin in the northwest Yangtze Block, South China
The Ediacaran to Cambrian in the northwest Yangtze Block, has long been considered to be formed in a passive margin. Wells and seismic data, however, show that a Lower Cambrian thi...
Coevolution of Brachiopod Paleobiogeography and Tectonopaleogeography during the Early–Middle Permian
Coevolution of Brachiopod Paleobiogeography and Tectonopaleogeography during the Early–Middle Permian
AbstractA comprehensive compilation and systematic analysis of known early and middle Permian brachiopod faunas shows that the early Permian brachiopod faunas comprise three realms...
Sedimentary provenance analysis unravels the Early Cambrian orogeny in the NW Yangtze Block, South China
Sedimentary provenance analysis unravels the Early Cambrian orogeny in the NW Yangtze Block, South China
The Ediacaran to Cambrian transition witnessed a key interval in the Earth’s history for biological revolution, environmental change and tectonic evolution. Wells and sei...

Back to Top