Earliest siphuncle-bearing cephalopod from the early Cambrian
Data files
Mar 10, 2026 version files 3.26 GB
-
20231122_gjf_Bar297-1_3.72um-tiff.zip
1.04 GB
-
20260106_gjf_cupi-7_2.72um_tiff.zip
1.08 GB
-
20260107_gjf_cupi-11_2.04um_tiff.zip
1.13 GB
-
README.md
1.01 KB
Mar 10, 2026 version files 3.26 GB
-
20231122_gjf_Bar297-1_3.72um-tiff.zip
1.04 GB
-
20260106_gjf_cupi-7_2.72um_tiff.zip
1.08 GB
-
20260107_gjf_cupi-11_2.04um_tiff.zip
1.13 GB
-
README.md
1.01 KB
Apr 06, 2026 version files 3.26 GB
-
20231122_gjf_Bar297-1_3.72um-tiff.zip
1.04 GB
-
20260106_gjf_eosceras-7_2.72um_tiff.zip
1.08 GB
-
20260107_gjf_eosceras-11_2.04um_tiff.zip
1.13 GB
-
README.md
1.01 KB
May 22, 2026 version files 3.26 GB
-
20231122_gjf_Bar297-1_3.72um-tiff.zip
1.04 GB
-
20260106_gjf_eoceras-7_2.72um_tiff.zip
1.08 GB
-
20260107_gjf_eoceras-11_2.04um_tiff.zip
1.13 GB
-
README.md
1.05 KB
Abstract
Modern cephalopods are unique among molluscs in ancestrally possessing chambered, gas- and fluid-filled shells, the internal septa of which are penetrated by a siphuncle. Combined with jet propulsion, the siphuncle enables cephalopods to engage in a nektonic and mostly predatory lifestyle through long-term regulation of their bouyancy. The origin of this key innovation remains enigmatic, as major gaps exist between the earliest accepted cephalopod, Plectronoceras cambria from the late Cambrian, and molecular clock estimates placing the lineage’s divergence from other molluscs in the early Cambrian. Here we report Eoceras shaanxiense gen. et sp. nov., a millimetre-sized cephalopod with an orthoconic shell from the Shuijingtuo Formation (Cambrian Stage 3) of South China. Internally, the shell exhibits multiple septa along with a peripherally situated segmented tube that appears to bridge the septa through minute canals, indicating that the soft body migrated aperturally to form successive chambers during growth while maintaining contact with earlier chambers via the tube. Collectively, these features identify the segmented tube in Eoceras gen. nov. as a candidate primordial cephalopod siphuncle, thus extending the known range of stem cephalopods back to the early Cambrian and also revealing the early stages in the evolutionary assembly of a chambered phragmocone employed in buoyancy regulation.
Dataset DOI: 10.5061/dryad.qbzkh18zk
Description of the data and file structure
Micro-CT scanning data was performed on a single coated specimen CUBar297 (GQ-LYB-4)-1(20231122_gjf_Bar297-1_3.72um-tiff.zip), and two uncoated specimens CU(CT-eosceras)-7(20260106_gjf_eoceras-7_2.72um_tiff.zip) and CU(CT-eosceras)-11(20260107_gjf_eoceras-11_2.04um_tiff.zip) with the Zeiss Xradia 520 system at the State Key Laboratory of Continental Dynamics of Northwest University in Xi’an, Shaanxi Province, China.
Scanning conditions were 40 kV accelerating voltage, 80 μA beam current, and an isotropic voxel size of 3.72 μm, 2.72 μm and 2.04 μm, respectively. Approximately 1,000 projection images were acquired in TIFF format. Data were reconstructed using standard, filtered back-projection algorithms and visualized in VG Studio Max 2.2 for three-dimensional volume rendering and segmentation.
Code/software
VG Studio Max 2.2
Changes after Mar 10, 2026: We changed the files name.
Changes after Apr 6, 2026: We changed the files name.
