@misc{dutton1882tertiary1,
    author = "Dutton, C. E",
    title = "Tertiary History of the Grand Canyon District",
    year = "1882",
    howpublished = "Washington, D.C., Government Printing Office, v. 2, 264 p.; United States Geological Survey Mongraphs",
    note = "talkorigins\_source = {true}; raw\_reference = {Dutton, C. E., 1882, Tertiary History of the Grand Canyon District: Washington, D.C., Government Printing Office, v. 2, 264 p.; United States Geological Survey Mongraphs.}"
}

@article{gude1915mollusca,
    author = "Gude, G. K.",
    title = "Mollusca, IV: Helicidae Genus Plectopylis",
    year = "1915",
    journal = "Records of the Zoological Survey of India",
    abstract = "No Abstract.",
    url = "https://doi.org/10.26515/rzsi/v116/i2/1915/163689",
    doi = "10.26515/rzsi/v116/i2/1915/163689",
    pages = "505-513"
}

@article{crossref1934some,
    title = "SOME NEW ZEALAND TERTIARY MOLLUSCA",
    year = "1934",
    journal = "Journal of Molluscan Studies",
    url = "https://doi.org/10.1093/oxfordjournals.mollus.a064208",
    doi = "10.1093/oxfordjournals.mollus.a064208"
}

@misc{macneil1965evolution,
    author = "MacNeil, F. Stearns",
    title = "Evolution and distribution of the genus Mya, and Tertiary migrations of Mollusca",
    year = "1965",
    booktitle = "Professional Paper",
    url = "https://doi.org/10.3133/pp483g",
    doi = "10.3133/pp483g"
}

@misc{macneil1965evolution4,
    author = "MacNeil, F. S",
    title = "Evolution of the genus Mya, and Tertiary migrations of Mollusca",
    year = "1965",
    howpublished = "United States Geological Survey, Professional Paper, v. 483-G, p. G1-G51",
    note = "talkorigins\_source = {true}; raw\_reference = {MacNeil, F. S., 1965, Evolution of the genus Mya, and Tertiary migrations of Mollusca: United States Geological Survey, Professional Paper, v. 483-G, p. G1-G51.}"
}

@misc{waller1969the6,
    author = "Waller, T. R",
    title = "The evolution of the Argopecten gibbus stock (Mollusca",
    year = "1969",
    howpublished = "Bivalvia), with emphasis on the Tertiary and Quaternary of eastern North America: Paleontological Society Memoirs, v. 3, p. 1-125",
    note = "talkorigins\_source = {true}; raw\_reference = {Waller, T. R., 1969, The evolution of the Argopecten gibbus stock (Mollusca: Bivalvia), with emphasis on the Tertiary and Quaternary of eastern North America: Paleontological Society Memoirs, v. 3, p. 1-125.}"
}

@inproceedings{gartner1971phylogenetic2,
    author = "Gartner, S. and Jr",
    title = "Phylogenetic lineages in the Lower Tertiary coccolith genus Chiasmolithus",
    year = "1971",
    booktitle = "North American Paleontological Convention, Proceedings, p. 930-957; Part G",
    note = "talkorigins\_source = {true}; raw\_reference = {Gartner, S., Jr., 1971, Phylogenetic lineages in the Lower Tertiary coccolith genus Chiasmolithus: North American Paleontological Convention, Proceedings, p. 930-957; Part G.}"
}

@article{moore1972midtertiary,
    author = "Moore, T. C.",
    title = "Mid-Tertiary Evolution of the Radiolarian Genus Calocycletta",
    year = "1972",
    journal = "Micropaleontology",
    url = "https://doi.org/10.2307/1484991",
    doi = "10.2307/1484991",
    number = "2",
    pages = "144",
    volume = "18"
}

@book{parker1977lower5,
    author = "Parker, J. R",
    title = "Lower Tertiary sand development in the central North Sea, in Developments in Petroleum Geology",
    year = "1977",
    publisher = "Essex, England, Applied Science Publications, Limited, v. 1, p. 447-453",
    note = "talkorigins\_source = {true}; raw\_reference = {Parker, J. R., 1977, Lower Tertiary sand development in the central North Sea, in Developments in Petroleum Geology: Essex, England, Applied Science Publications, Limited, v. 1, p. 447-453.}"
}

@book{leipzig1982stratigraphy3,
    author = "Leipzig, M. R",
    title = "Stratigraphy, Sedimentation and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland Formation, Kirtland Shale and Early Tertiary Ojo Alamo Sandstone; Eastern San Juan Basin, New Mexico [MS dissert.]",
    year = "1982",
    publisher = "University of Wisconsin-Milwaukee, 555 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1982, Stratigraphy, Sedimentation and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland Formation, Kirtland Shale and Early Tertiary Ojo Alamo Sandstone; Eastern San Juan Basin, New Mexico [MS dissert.]: University of Wisconsin-Milwaukee, 555 p.}"
}

@article{baryosef1987mollusca,
    author = "Bar-Yosef, Daniella E. and Heller, Joseph",
    title = "Mollusca from Yiftah'el, Lower Galilee, Israel",
    year = "1987",
    journal = "Paléorient",
    abstract = "Sur le site PPNB de Yitfah'el, l'assemblage de coquilles marines ressemble à celui des autres sites PPNB.'prédominance de bivalves marins, quelques cauries et deux coquilles de la Mer Rouge. La plupart des coquilles d'eau douce furent probablement apportées dans l'argile qui servit à confectionner les briques crues alors que les escargots terrestres semblent avoir envahi le site après sa désertion. Les coquilles marines du Néolithique récent et du Bronze I sont très peu nombreuses et leur contexte stratigraphique pas très clair.",
    url = "https://doi.org/10.3406/paleo.1987.4425",
    doi = "10.3406/paleo.1987.4425",
    number = "1",
    pages = "131-135",
    volume = "13"
}

@article{gerlach1999snails,
    author = "Gerlach, Justin",
    title = "Snails of the genus Pachnodus (Mollusca; Gastropoda; Enidae): their origins and evolution",
    year = "1999",
    journal = "Journal of Biogeography",
    abstract = "Summary Aim The phylogeny of the enid land‐snail genus Pachnodus was determined in order to provide information on biogeographical patterns within the granitic Seychelles islands. Location The genus Pachnodus is endemic to the granitic islands of Seychelles (Mahé, Silhouette, Praslin, La Digue and Fregate). Methods Phylogeny was determined using a cladistic analysis of nineteen shell and soft‐body anatomy characters. The outgroup used was the central‐east African genus Cerastus. Results The proposed phylogeny indicates that the genus divided into two distinct subgenera early in its history. Subsequent speciation occurred in parallel in the two subgenera, resulting in several islands supporting at least two distinct species representing the two subgenera. Main conclusions The pattern of speciation is largely explicable by vicariance as a result of sea‐level rises, followed by habitat specialisation and further speciation. The pattern is in contrast to previously published scenarios for other taxa in the islands and indicates significant differences between evolutionary and habitat factors in the biogeography of the Seychelles fauna",
    url = "https://doi.org/10.1046/j.1365-2699.1999.00259.x",
    doi = "10.1046/j.1365-2699.1999.00259.x",
    number = "2",
    pages = "251-255",
    volume = "26"
}

@article{kříž2007origin,
    author = "KŘÍŽ, JIŘÍ",
    title = "ORIGIN, EVOLUTION AND CLASSIFICATION OF THE NEW SUPERORDER NEPIOMORPHIA (MOLLUSCA, BIVALVIA, LOWER PALAEOZOIC)",
    year = "2007",
    journal = "Palaeontology",
    abstract = "A number of bivalve taxa defined in the past as ‘Cryptodonten’ by Neumayr, 1884 were grouped together in the high‐level taxon Palaeoconchae Neumayr, 1884. Cox (1969) noted that Palaeoconchae and Cryptodonta were synonymous and Newell (1969) used Cryptodonta as a subclass of bivalves. However, for the past 120 years, the Cryptodonta has been poorly conceptualized and the name was used for poorly understood genera or those lacking dentition. As used by Newell, Cryptodonta included taxa now placed in the subclasses Protobranchia Pelseneer and Autolamellibranchiata Grobben, and to the class Rostroconchia Pojeta, Runnegar, Morris and Newell. The bulk of Newell's use of Cryptodonta was made up of Silurian and Devonian taxa first described by Barrande (1881) from Bohemia; Newell placed these in the order Praecardioida Newell. In effect, Cryptodonta became a ‘wastebasket’ grouping for what, at the time, were poorly understood taxa. Many of the formerly poorly understood praecardioids are now better known and are herein placed in the new superorder Nepiomorphia. The Nepiomorphia contains two orders: (1) order Praecardioida that includes the families Slavidae Kříž, Cardiolidae Hoernes, Praecardiidae Hoernes and Buchiolidae Grimm; and (2) new order Antipleuroida that includes the families Stolidotidae fam. nov., Spanilidae fam. nov. and Antipleuridae Neumayr. The Nepiomorphia originated probably in the early Silurian as result of r‐selection progenesis. When the marine current system became re‐established after the late Ordovician glaciation and in the early Silurian, an at least temporary ventilation of the shallow waters by surface currents was renewed in higher latitudes of peri‐Gondwana and Siberia, producing acceptable sea‐bottom environments. Larvae were distributed by surface currents from the warm tropical regions of Laurentia and Baltica and were among the first benthic organisms to colonize the new environments. Temporary ventilation created frequent density‐independent catastrophic mortalities of early ontogenetic stages, with no competitors and with super‐abundant resources. During the Silurian and early Devonian, the Nepiomorphia underwent several diversifications in the recurring cephalopod limestone biofacies characteristic of peri‐Gondwana, and evolved infaunal, semi‐infaunal and epifaunal modes of life in several lineages. The Nepiomorphia most probably became extinct during the early Carboniferous and had no role in the future evolution of the Bivalvia.",
    url = "https://doi.org/10.1111/j.1475-4983.2007.00720.x",
    doi = "10.1111/j.1475-4983.2007.00720.x",
    number = "6",
    pages = "1341-1365",
    volume = "50"
}

@incollection{crossref2014lower,
    title = "Lower Tertiary",
    year = "2014",
    booktitle = "Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik",
    url = "https://doi.org/10.1007/978-3-642-41714-6\_122512",
    doi = "10.1007/978-3-642-41714-6\_122512",
    pages = "824-824"
}