Data from: Exceptional preservation and unexpected diversity of radiolarians in the aftermath of the Permian-Triassic mass extinction
Data files
Jun 03, 2026 version files 257.37 MB
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06_001.tif
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06_010.tif
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lD23_06_01.tif
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README.md
1.94 KB
Abstract
The Early Triassic is typically described as an interval of poor fossil preservation and low diversity in the aftermath of the Permian–Triassic mass extinction. For radiolarians, very little information is available due to the lack of known radiolarian-yielding locations. Yet, here well-preserved radiolarians, including the oldest (Griesbachian, Early Triassic) occurrence of fossilized central capsule membranes, are described from a shallow marine Permian/Triassic boundary succession at Lusitaniadalen (Svalbard). Eleven species from seven radiolaria genera have been found, including three new species (Entactinia sengeri n. sp., Archaeocenosphaera plankei n. sp. and Thaisphaera ullarinmanae n. sp.) and two new subspecies (Entactinia meishanensis smyraksikorae n. subsp. and Grandetortura nipponica stepheni n. subsp.). Combined with the unexpectedly high diversity of other organisms from the Permian/Triassic boundary in Svalbard this new data further indicates that Svalbard represents either a previously unknown refuge or somewhere with exceptional preservation in the aftermath of the mass extinction event.
Dataset DOI: 10.5061/dryad.pzgmsbd39
Description of the data and file structure
SEM images of radiolarian specimens from Permian–Triassic sediments from the Stensiöfjellet member of the Kapp Starostin Formation and the Deltadalen member of the Vikinghøgda Formation, Svalbard. The samples come from the Lusitaniadalen section (78.2986°N, 16.7331°E), a valley on the northwestern side of Sassendalen, Spitsbergen. Samples are taken from concretionary levels LD23-06 and LD23-07.
The radiolarian specimens and the central capsule membranes of the Lusitaniadalen section, have been accessioned at the Hungarian Natural History Museum in Budapest, Hungary (INV 2025.142-162) and at the Natural History Museum, University of Oslo (PMO 250.522/06; 250.525/98; 250.525/122).
Samples are taken from concretionary levels LD23-06
06_001.tif
06_010.tif
06_010b.tif
06_010c.tif
06_010d.tif
06_015.tif
06_017.tif
06_020.tif
06_022.tif
06_022b.tif
06_023.tif
06_025.tif
06_026.tif
06_028.tif
06_029.tif
06_031.tif
06_032.tif
06_033.tif
06_039.tif
06_039b.tif
06_040.tif
06_040b.tif
06_040c.tif
06_041.tif
06_042.tif
06_044.tif
06_044b.tif
06_045.tif
06_46.tif
lD23_06_01.tif
lD23_06_09.tif
lD23_06_12.tif
lD23_06_21.tif
lD23_06_22.tif
lD23_06_26.tif
lD23_06_27.tif
lD23_06_63.tif
lD23_06_67.tif
lD23_06_67_1.tif
Samples are taken from concretionary levels LD23-07
LD_23_07_001.tif
LD_23_07_002.tif
LD_23_07_003.tif
LD_23_07_004.tif
LD23_07_005.tif
LD23_07_005b.tif
LD23_07_005c.tif
LD23_07_005d.tif
LD23_07_007.tif
LD23_07_008.tif
LD23_07_009b.tif
LD23_07_009c.tif
LD23_07_012.tif
LD23_07_021.tif
LD23_07_021b.tif
LD23_07_024.tif
LD23_07_027.tif
LD23_07_027b.tif
LD23_07_037.tif
LD23_07_038.tif
See the publication for the appropriate horizon of the samples.
