<i>Himatiichnus mangano</i> igen. et isp. nov., a scalidophoran trace fossil from the late Ediacaran of Namibia

<i>Himatiichnus mangano</i> igen. et isp. nov., a new trace fossil from the late Ediacaran Huns Member of the Urusis Formation, southern Namibia, comprises intertwining tubes exhibiting dual lineation patterns and reminiscent of both modern and early Cambrian examples of priapulid worm burrows. These similarities support the interpretation of a total-group scalidophoran tracemaker for <i>H. mangano</i>, thus providing direct evidence for the first appearance date of Scalidophora in the late Ediacaran <i>ca</i> 539 Ma. This new material is thus indicative of the presence of total-group scalidophorans below the Cambrian boundary and supports inference of a lengthy Precambrian fuse for the Cambrian explosion.

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Publication Details

Journal
Royal Society Open Science
Published
2024-10-01
DOI
https://doi.org/10.1098/rsos.240452
Citations
6
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
9.53

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article

Himatiichnus mangano igen. et isp. nov., a scalidophoran trace fossil from the late Ediacaran of Namibia

Marc Laflamme, Simon A.F. Darroch, Helke Mocke, Katherine A. Turk et al.
6 citations
Royal Society Open Science
Paleontology and Stratigraphy of Fossils
9.53
article

Himatiichnus mangano igen. et isp. nov., a scalidophoran trace fossil from the late Ediacaran of Namibia

Marc Laflamme, Simon A.F. Darroch, Helke Mocke, Katherine A. Turk, Mikaela A. Pulsipher
article en
6 citations

Abstract

<i>Himatiichnus mangano</i> igen. et isp. nov., a new trace fossil from the late Ediacaran Huns Member of the Urusis Formation, southern Namibia, comprises intertwining tubes exhibiting dual lineation patterns and reminiscent of both modern and early Cambrian examples of priapulid worm burrows. These similarities support the interpretation of a total-group scalidophoran tracemaker for <i>H. mangano</i>, thus providing direct evidence for the first appearance date of Scalidophora in the late Ediacaran <i>ca</i> 539 Ma. This new material is thus indicative of the presence of total-group scalidophorans below the Cambrian boundary and supports inference of a lengthy Precambrian fuse for the Cambrian explosion.

Royal Society Open ScienceVol. 11(10)
National Park Service (US), University of Toronto (CA), Vanderbilt University (US), Senckenberg Research Institute and Natural History Museum Frankfurt/M (DE), Geological Survey of Namibia (NA), Institut de Biologia Evolutiva (ES), University of Missouri (US)
National Science Foundation, Vanderbilt University, Paleontological Society, Sight Research UK, Natural Sciences and Engineering Research Council of Canada, Natural Environment Research Council, Division of Environmental Biology, Division of Earth Sciences
Life below water
Openalex Percentile: Top 3%
Paleontology and Stratigraphy of Fossils
9.53
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