@article{GeyerLanding2021,
  author    = {Geyer, Gerd and Landing, Ed},
  title     = {The Souss lagerstatte of the Anti-Atlas, Morocco: discovery of the first Cambrian fossil lagerstatte from Africa},
  series = {Scientific Reports},
  volume    = {11},
  journal   = {Scientific Reports},
  number    = {1},
  doi       = {10.1038/s41598-021-82546-0},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-259236},
  pages     = {3107},
  year      = {2021},
  abstract  = {Episodic low oxygenated conditions on the sea-floor are likely responsible for exceptional preservation of animal remains in the upper Amouslek Formation (lower Cambrian, Stage 3) on the northern slope of the western Anti-Atlas, Morocco. This stratigraphic interval has yielded trilobite, brachiopod, and hyolith fossils with preserved soft parts, including some of the oldest known trilobite guts. The "Souss fossil lagerstatte" (newly proposed designation) represents the first Cambrian fossil lagerstatte in Cambrian strata known from Africa and is one of the oldest trilobite-bearing fossil lagerstatten on Earth. Inter-regional correlation of the Souss fossil lagerstatte in West Gondwana suggests its development during an interval of high eustatic levels recorded by dark shales that occur in informal upper Cambrian Series 2 in Siberia, South China, and East Gondwana.},
  language  = {en}
}
@article{LandingGeyerSchmitzetal.2021,
  author    = {Landing, Ed and Geyer, Gerd and Schmitz, Mark D. and Wotte, Thomas and Kouchinsky, Artem},
  title     = {(Re)proposal of three Cambrian Subsystems and their Geochronology},
  series = {Episodes},
  volume    = {44},
  journal   = {Episodes},
  doi       = {https://doi.org/10.18814/epiiugs/2020/020088},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-363144},
  pages     = {273-283},
  year      = {2021},
  abstract  = {The Cambrian is anomalous among geological systems as many reports divide it into three divisions of indeterminate rank. This use of "lower", "middle", and "upper" has been a convenient way to subdivide the Cambrian despite agreement it consists of four global series. Traditional divisions of the system into regional series (Lower, Middle, Upper) reflected local biotic developments not interprovincially correlatable with any precision. However, use of "lower", "middle", and "upper" is unsatisfactory. These adjectives lack standard definition, evoke the regional series, and are misused. Notably, there is an almost 50 year use of three Cambrian subsystems and a 1997 proposal to divide the Avalonian and global Cambrian into four series and three subsystems. The global series allow proposal of three formal subsystems: a ca. 32.6 Ma Lower Cambrian Subsystem (Terreneuvian and Series 2/proposed Lenaldanian Series), a ca. 9.8 Ma Middle, and a ca. 10 Ma Upper Cambrian Subsystem (=Furongian Series). Designations as "Lower Cambrian Subsystem" or "global Lower Cambrian" distinguish the new units from such earlier units as "Lower Cambrian Series" and substitute for the de facto subsystem terms "lower", "middle", and "upper". Cambrian subsystems are comparable to the Carboniferous' Lower (Mississippian) and Upper (Pennsylvanian) Subsystems.},
  language  = {en}
}
@article{GeyerLandingMeieretal.2023,
  author    = {Geyer, Gerd and Landing, Ed and Meier, Stefan and H{\"o}hn, Stefan},
  title     = {Oldest known West Gondwanan graptolite: Ovetograptus? sp. (lower Agdzian/lowest Wuliuan; basal Middle Cambrian) of the Franconian Forest, Germany, and review of pre-Furongian graptolithoids},
  series = {Pal{\"a}ontologische Zeitschrift},
  volume    = {97},
  journal   = {Pal{\"a}ontologische Zeitschrift},
  number    = {4},
  issn      = {0031-0220},
  doi       = {10.1007/s12542-022-00627-5},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-324099},
  pages     = {677-686},
  year      = {2023},
  abstract  = {The occurrence of a likely graptolite in lowest Wuliuan strata of the Franconian Forest almost certainly records the oldest known graptolithoid hemichordate in West Gondwana and possibly the oldest graptolite presently known. The fossil is a delicate, erect, apparently unbranched rhabdosome with narrow thecae tentatively assigned to the poorly known genus Ovetograptus of the Dithecodendridae. This report includes an overview of pre-Furongian graptolithoids with slight corrections on the stratigraphic position of earlier reported species.},
  language  = {en}
}