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Treatise on Invertebrate Paleontology

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The Treatise on Invertebrate Paleontology (or TIP) published by the Geological Society of America and the University of Kansas Press, is a definitive multi-authored work of some 50 volumes, written by more than 300 paleontologists, and covering every phylum, class, order, family, and genus of fossil and extant (still living) invertebrate animals. The prehistoric invertebrates are described as to their taxonomy, morphology, paleoecology, stratigraphic and paleogeographic range. However, taxa with no fossil record whatsoever have just a very brief listing.

Publication of the decades-long Treatise on Invertebrate Paleontology is a work-in-progress; and therefore it is not yet complete: For example, there is no volume yet published regarding the post-Paleozoic era caenogastropods (a molluscan group including the whelk and periwinkle). Furthermore, every so often, previously published volumes of the Treatise are revised.

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Geological Society of America

Geological Society of America

The Geological Society of America (GSA) is a nonprofit organization dedicated to the advancement of the geosciences.

University of Kansas

University of Kansas

The University of Kansas (KU) is a public research university with its main campus in Lawrence, Kansas. Two branch campuses are in the Kansas City metropolitan area on the Kansas side: the university's medical school and hospital in Kansas City, Kansas, the Edwards Campus in Overland Park. There are also educational and research sites in Garden City, Hays, Leavenworth, Parsons, and Topeka, an agricultural education center in rural north Douglas County, and branches of the medical school in Salina and Wichita. The university is a member of the Association of American Universities and is classified among "R1: Doctoral Universities – Very high research activity".

Genus

Genus

Genus is a taxonomic rank used in the biological classification of living and fossil organisms as well as viruses. In the hierarchy of biological classification, genus comes above species and below family. In binomial nomenclature, the genus name forms the first part of the binomial species name for each species within the genus.E.g. Panthera leo (lion) and Panthera onca (jaguar) are two species within the genus Panthera. Panthera is a genus within the family Felidae.

Fossil

Fossil

A fossil is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the fossil record.

Invertebrate

Invertebrate

Invertebrates are a paraphyletic group of animals that neither possess nor develop a vertebral column, derived from the notochord. This is a grouping including all animals apart from the chordate subphylum Vertebrata. Familiar examples of invertebrates include arthropods, mollusks, annelids, echinoderms and cnidarians.

Taxonomy (biology)

Taxonomy (biology)

In biology, taxonomy is the scientific study of naming, defining (circumscribing) and classifying groups of biological organisms based on shared characteristics. Organisms are grouped into taxa and these groups are given a taxonomic rank; groups of a given rank can be aggregated to form a more inclusive group of higher rank, thus creating a taxonomic hierarchy. The principal ranks in modern use are domain, kingdom, phylum, class, order, family, genus, and species. The Swedish botanist Carl Linnaeus is regarded as the founder of the current system of taxonomy, as he developed a ranked system known as Linnaean taxonomy for categorizing organisms and binomial nomenclature for naming organisms.

Morphology (biology)

Morphology (biology)

Morphology is a branch of biology dealing with the study of the form and structure of organisms and their specific structural features.

Paleoecology

Paleoecology

Paleoecology is the study of interactions between organisms and/or interactions between organisms and their environments across geologic timescales. As a discipline, paleoecology interacts with, depends on and informs a variety of fields including paleontology, ecology, climatology and biology.

Stratigraphy

Stratigraphy

Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks. Stratigraphy has three related subfields: lithostratigraphy, biostratigraphy, and chronostratigraphy.

Caenogastropoda

Caenogastropoda

Caenogastropoda is a taxonomic subclass of molluscs in the class Gastropoda. It is a large diverse group which are mostly sea snails and other marine gastropod mollusks, but also includes some freshwater snails and some land snails. The subclass is the most diverse and ecologically successful of the gastropods.

Mollusca

Mollusca

Mollusca is the second-largest phylum of invertebrate animals after the Arthropoda, the members of which are known as molluscs or mollusks. Around 85,000 extant species of molluscs are recognized. The number of fossil species is estimated between 60,000 and 100,000 additional species. The proportion of undescribed species is very high. Many taxa remain poorly studied.

Common periwinkle

Common periwinkle

The common periwinkle or winkle is a species of small edible whelk or sea snail, a marine gastropod mollusc that has gills and an operculum, and is classified within the family Littorinidae, the periwinkles.

Evolution of the project

Raymond C. Moore, the project's founder and first editor, originally envisioned this Treatise in invertebrate paleontology as comprising just three large volumes, and totaling only three thousand pages.

The project began with work on a few, mostly slim volumes in which a single senior specialist in a distinct field of invertebrate paleozoology would summarize one particular group. As a result, each publication became a comprehensive compilation of everything known at that time for each group. Examples of this stage of the project are Part G. Bryozoa, by Ray S. Bassler (the first volume, published in 1953), and Part P. Arthropoda Part 2, the Chelicerata by Alexander Petrunkevitch (1955/1956).

Around 1959 or 1960, as more and larger invertebrate groups were being addressed, the incompleteness of the then-current state of affairs became apparent. So several senior editors of the Treatise started major research programs to fill in the evident gaps. Consequently, the succeeding volumes, while still maintaining the original format, began to change from being a set of single-authored compilations into being major research projects in their own right. Newer volumes had a committee and a chief editor for each volume, with yet other authors and researchers assigned particular sections. Museum collections that had not been previously described were studied; and sometimes new major taxonomic families—and even orders—had to be described. More attention was given to transitional fossils and evolutionary radiation—eventually producing a much-more complete encyclopedia of invertebrate paleontology.

But even in the second set of volumes, the various taxa were still described and organized in a classical Linnaean sense. The more-recent volumes began to introduce phylogenetic and cladistic ideas, along with new developments and discoveries in fields such as biogeography, molecular phylogeny, paleobiology, and organic chemistry, so that the current edition of Brachiopoda (1997 to 2002) is classified according to a cladistic arrangement, with three subphyla and a large number of classes replacing the original two classes of Articulata and Inarticulata.

All these discoveries led to revisions and additional volumes. Even those taxa already covered were expanded: Books such as those regarding the Cnidaria (vol. F), the Brachiopoda (vol. H) and the Trilobita (vol. O) each went from one modest publication to three large volumes. And yet another volume regarding the brachiopods (number five) was published in 2006.

Until 2007, the editor of the Treatise was Roger L. Kaesler at The Paleontological Institute at the University of Kansas in Lawrence, Kansas.

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Editing

Editing

Editing is the process of selecting and preparing written, photographic, visual, audible, or cinematic material used by a person or an entity to convey a message or information. The editing process can involve correction, condensation, organisation, and many other modifications performed with an intention of producing a correct, consistent, accurate and complete piece of work.

Invertebrate paleontology

Invertebrate paleontology

Invertebrate paleontology is sometimes described as invertebrate paleozoology or invertebrate paleobiology. Whether it is considered to be a subfield of paleontology, paleozoology, or paleobiology, this discipline is the scientific study of prehistoric invertebrates by analyzing invertebrate fossils in the geologic record.

Paleozoology

Paleozoology

Palaeozoology, also spelled as Paleozoology, is the branch of paleontology, paleobiology, or zoology dealing with the recovery and identification of multicellular animal remains from geological contexts, and the use of these fossils in the reconstruction of prehistoric environments and ancient ecosystems.

Bryozoa

Bryozoa

Bryozoa are a phylum of simple, aquatic invertebrate animals, nearly all living in sedentary colonies. Typically about 0.5 millimetres long, they have a special feeding structure called a lophophore, a "crown" of tentacles used for filter feeding. Most marine bryozoans live in tropical waters, but a few are found in oceanic trenches and polar waters. The bryozoans are classified as the marine bryozoans (Stenolaemata), freshwater bryozoans (Phylactolaemata), and mostly-marine bryozoans (Gymnolaemata), a few members of which prefer brackish water. 5,869 living species are known. At least two genera are solitary ; the rest are colonial.

Chelicerata

Chelicerata

The subphylum Chelicerata constitutes one of the major subdivisions of the phylum Arthropoda. It contains the sea spiders, horseshoe crabs, and arachnids, as well as a number of extinct lineages, such as the eurypterids and chasmataspidids.

Alexander Petrunkevitch

Alexander Petrunkevitch

Alexander Ivanovitch Petrunkevitch was an eminent Russian arachnologist of his time. From 1910 to 1939 he described over 130 spider species. One of his most famous essays was "The Spider and the Wasp." In it he uses effective word choices and some comic touch.

Museum

Museum

A museum is a building or institution that cares for and displays a collection of artifacts and other objects of artistic, cultural, historical, or scientific importance. Many public museums make these items available for public viewing through displays that may be permanent or temporary. The largest museums are located in major cities throughout the world, while thousands of local museums exist in smaller cities, towns, and rural areas. Museums have varying aims, ranging from the conservation and documentation of their collection, serving researchers and specialists, to catering to the general public. The goal of serving researchers is not only scientific, but intended to serve the general public.

Evolution

Evolution

In biology, evolution is the change in heritable characteristics of biological populations over successive generations. These characteristics are the expressions of genes, which are passed on from parent to offspring during reproduction. Variation tends to exist within any given population as a result of genetic mutation and recombination. Evolution occurs when evolutionary processes such as natural selection and genetic drift act on this variation, resulting in certain characteristics becoming more common or more rare within a population. The evolutionary pressures that determine whether a characteristic is common or rare within a population constantly change, resulting in a change in heritable characteristics arising over successive generations. It is this process of evolution that has given rise to biodiversity at every level of biological organisation.

Encyclopedia

Encyclopedia

An encyclopedia or encyclopædia is a reference work or compendium providing summaries of knowledge either general or special to a particular field or discipline. Encyclopedias are divided into articles or entries that are arranged alphabetically by article name or by thematic categories, or else are hyperlinked and searchable. Encyclopedia entries are longer and more detailed than those in most dictionaries. Generally speaking, encyclopedia articles focus on factual information concerning the subject named in the article's title; this is unlike dictionary entries, which focus on linguistic information about words, such as their etymology, meaning, pronunciation, use, and grammatical forms.

Linnaean taxonomy

Linnaean taxonomy

Linnaean taxonomy can mean either of two related concepts:The particular form of biological classification (taxonomy) set up by Carl Linnaeus, as set forth in his Systema Naturae (1735) and subsequent works. In the taxonomy of Linnaeus there are three kingdoms, divided into classes, and they, in turn, into lower ranks in a hierarchical order. A term for rank-based classification of organisms, in general. That is, taxonomy in the traditional sense of the word: rank-based scientific classification. This term is especially used as opposed to cladistic systematics, which groups organisms into clades. It is attributed to Linnaeus, although he neither invented the concept of ranked classification nor gave it its present form. In fact, it does not have an exact present form, as "Linnaean taxonomy" as such does not really exist: it is a collective (abstracting) term for what actually are several separate fields, which use similar approaches.

Cladistics

Cladistics

Cladistics is an approach to biological classification in which organisms are categorized in groups ("clades") based on hypotheses of most recent common ancestry. The evidence for hypothesized relationships is typically shared derived characteristics (synapomorphies) that are not present in more distant groups and ancestors. However, from an empirical perspective, common ancestors are inferences based on a cladistic hypothesis of relationships of taxa whose character states can be observed. Theoretically, a last common ancestor and all its descendants constitute a (minimal) clade. Importantly, all descendants stay in their overarching ancestral clade. For example, if the terms worms or fishes were used within a strict cladistic framework, these terms would include humans. Many of these terms are normally used paraphyletically, outside of cladistics, e.g. as a 'grade', which are fruitless to precisely delineate, especially when including extinct species. Radiation results in the generation of new subclades by bifurcation, but in practice sexual hybridization may blur very closely related groupings.

Biogeography

Biogeography

Biogeography is the study of the distribution of species and ecosystems in geographic space and through geological time. Organisms and biological communities often vary in a regular fashion along geographic gradients of latitude, elevation, isolation and habitat area. Phytogeography is the branch of biogeography that studies the distribution of plants. Zoogeography is the branch that studies distribution of animals. Mycogeography is the branch that studies distribution of fungi, such as mushrooms.

Layout of the articles

From the beginning, the character of the Treatise volumes has followed and further developed the pattern of the classic Invertebrate Paleontology written by Moore, Lalicker and Fischer (1953).

Following their lead, the Treatise includes in a typical article (a) a description of the basic anatomy of the modern members of each invertebrate group, (b) distinctive features of the fossils, (c) a comprehensive illustrated glossary of terms, (d) a short discussion of the evolutionary history of the group, (e) a stratigraphic range chart, done at the level of the major subdivision (lower, middle and upper) of each Geologic period.

This is followed by (f) a listing and technical description of every known genus, along with (g) geographic distribution (usually by continent only, but occasionally by country) and (h) stratigraphic range.

Next come (i) one or two representative species illustrated by line drawings (in the early volumes) or by black-and-white photographs (in subsequent volumes), each accompanied by an appropriate reference for that genus. Furthermore, each Treatise article includes (j) the date, authorship, and scientific history of the taxa.

Finally, there is (k) a comprehensive bibliography and list of references. Not only that, but the more recent volumes and revisions also include (l) new fossil and phylogenetic discoveries, (m) advances in numerical and cladistic methods, (n) analysis of the group's genome, (o) its molecular phylogeny, and so on.

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Anatomy

Anatomy

Anatomy is the branch of biology concerned with the study of the structure of organisms and their parts. Anatomy is a branch of natural science that deals with the structural organization of living things. It is an old science, having its beginnings in prehistoric times. Anatomy is inherently tied to developmental biology, embryology, comparative anatomy, evolutionary biology, and phylogeny, as these are the processes by which anatomy is generated, both over immediate and long-term timescales. Anatomy and physiology, which study the structure and function of organisms and their parts respectively, make a natural pair of related disciplines, and are often studied together. Human anatomy is one of the essential basic sciences that are applied in medicine.

Glossary

Glossary

A glossary also known as a vocabulary or clavis, is an alphabetical list of terms in a particular domain of knowledge with the definitions for those terms. Traditionally, a glossary appears at the end of a book and includes terms within that book that are either newly introduced, uncommon, or specialized. While glossaries are most commonly associated with non-fiction books, in some cases, fiction novels sometimes include a glossary for unfamiliar terms.

Species

Species

In biology, a species is often defined as the largest group of organisms in which any two individuals of the appropriate sexes or mating types can produce fertile offspring, typically by sexual reproduction. It is the basic unit of classification and a taxonomic rank of an organism, as well as a unit of biodiversity. Other ways of defining species include their karyotype, DNA sequence, morphology, behaviour, or ecological niche. In addition, paleontologists use the concept of the chronospecies since fossil reproduction cannot be examined.

Photograph

Photograph

A photograph is an image created by light falling on a photosensitive surface, usually photographic film or an electronic image sensor, such as a CCD or a CMOS chip. Most photographs are now created using a smartphone/camera, which uses a lens to focus the scene's visible wavelengths of light into a reproduction of what the human eye would see. The process and practice of creating such images is called photography.

Taxon

Taxon

In biology, a taxon is a group of one or more populations of an organism or organisms seen by taxonomists to form a unit. Although neither is required, a taxon is usually known by a particular name and given a particular ranking, especially if and when it is accepted or becomes established. It is very common, however, for taxonomists to remain at odds over what belongs to a taxon and the criteria used for inclusion. If a taxon is given a formal scientific name, its use is then governed by one of the nomenclature codes specifying which scientific name is correct for a particular grouping.

Genome

Genome

In the fields of molecular biology and genetics, a genome is all the genetic information of an organism. It consists of nucleotide sequences of DNA. The nuclear genome includes protein-coding genes and non-coding genes, other functional regions of the genome such as regulatory sequences, and often a substantial fraction of 'junk' DNA with no evident function. Almost all eukaryotes have mitochondria and a small mitochondrial genome. Algae and plants also contain chloroplasts with a chloroplast genome.

List of its volumes

The following is an annotated list of the volumes already published (1953 to 2007) or volumes currently being prepared:

Introduction (A) and sub-metazoan Protista (B, C & D)

  • Part A. Introduction: Fossilization (Taphonomy), Biogeography, & Biostratigraphy. xxiii + 569 pages, 169 figures, 1979. ISBN 0-8137-3001-5. The original volume is out of print.[1]
  • Part B. Protoctista / Protista, Volume 1: Charophyta, Sub-volume 1, 2005. ISBN 0-8137-3002-3. ---- Parts B through D refer to mostly one-celled, nucleated forms of life, typically fossilized due to their siliceous tests. "Protista" and Protoctista" are nearly synonymous.[2]
  • Part C. Protista / Protoctista, Volume 2: Sarcodina, Chiefly "Thecamoebians" & Foraminiferida, Sub-volumes 1 and 2, xxxi + 900 p., 653 fig., 1964. ISBN 0-8137-3003-1.[4]
  • Part D. Protista / Protoctista, Volume 3: Protozoa (Chiefly Radiolaria & Tintinnina), xii + 195 p., 92 fig., 1954. ISBN 0-8137-3004-X. The original volume is out of print. [5]

Archaeocyatha and Porifera (E)

Cnidaria or Coelenterata (F)

Bryozoa (G)

  • Part G. Bryozoa, xii + 253 p., 175 fig., 1953. ISBN 0-8137-3007-4. The original volume is out-of-print. --- Part G refers to bryozoans, colonial animals also known as ectoprocts or moss animals.[13]

Brachiopoda (H)

Mollusca (I, J, K, L, M & N)

Arthropoda (O, P, Q & R)

Echinodermata (S, T & U)

Graptolithina (V)

Miscellanea and Conodonta (W)

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Fossil

Fossil

A fossil is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the fossil record.

Taphonomy

Taphonomy

Taphonomy is the study of how organisms decay and become fossilized or preserved in the paleontological record. The term taphonomy was introduced to paleontology in 1940 by Soviet scientist Ivan Efremov to describe the study of the transition of remains, parts, or products of organisms from the biosphere to the lithosphere.

Biogeography

Biogeography

Biogeography is the study of the distribution of species and ecosystems in geographic space and through geological time. Organisms and biological communities often vary in a regular fashion along geographic gradients of latitude, elevation, isolation and habitat area. Phytogeography is the branch of biogeography that studies the distribution of plants. Zoogeography is the branch that studies distribution of animals. Mycogeography is the branch that studies distribution of fungi, such as mushrooms.

Biostratigraphy

Biostratigraphy

Biostratigraphy is the branch of stratigraphy which focuses on correlating and assigning relative ages of rock strata by using the fossil assemblages contained within them. The primary objective of biostratigraphy is correlation, demonstrating that a particular horizon in one geological section represents the same period of time as another horizon at a different section. Fossils within these strata are useful because sediments of the same age can look completely different, due to local variations in the sedimentary environment. For example, one section might have been made up of clays and marls, while another has more chalky limestones. However, if the fossil species recorded are similar, the two sediments are likely to have been laid down around the same time. Ideally these fossils are used to help identify biozones, as they make up the basic biostratigraphy units, and define geological time periods based upon the fossil species found within each section.

Charophyta

Charophyta

Charophyta is a group of freshwater green algae, called charophytes, sometimes treated as a division, yet also as a superdivision or an unranked clade. The terrestrial plants, the Embryophyta emerged within Charophyta, possibly from terrestrial unicellular charophytes, with the class Zygnematophyceae as a sister group.

Test (biology)

Test (biology)

In biology, a test is the hard shell of some spherical marine animals and protists, notably sea urchins and microorganisms such as testate foraminiferans, radiolarians, and testate amoebae. The term is also applied to the covering of scale insects. The related Latin term testa is used for the hard seed coat of plant seeds.

Diatom

Diatom

A diatom is any member of a large group comprising several genera of algae, specifically microalgae, found in the oceans, waterways and soils of the world. Living diatoms make up a significant portion of the Earth's biomass: they generate about 20 to 50 percent of the oxygen produced on the planet each year, take in over 6.7 billion metric tons of silicon each year from the waters in which they live, and constitute nearly half of the organic material found in the oceans. The shells of dead diatoms can reach as much as a half-mile deep on the ocean floor, and the entire Amazon basin is fertilized annually by 27 million tons of diatom shell dust transported by transatlantic winds from the African Sahara, much of it from the Bodélé Depression, which was once made up of a system of fresh-water lakes.

Source: "Treatise on Invertebrate Paleontology", Wikipedia, Wikimedia Foundation, (2022, August 18th), https://en.wikipedia.org/wiki/Treatise_on_Invertebrate_Paleontology.

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References
  1. ^ Paleontological Institute. "Part A, Introduction". Treatise on Invertebrate Paleontology.
  2. ^ Paleontological Institute. "Part B, Protista 1, vol. 1". Treatise on Invertebrate Paleontology.
  3. ^ Paleontological Institute. "Part B, Protista 1, vol. 2". Treatise on Invertebrate Paleontology. Archived from the original on 9 October 2016. Retrieved 5 December 2013.
  4. ^ Paleontological Institute. "Part C, Protista 2, vol. 1 & 2". Treatise on Invertebrate Paleontology.
  5. ^ Paleontological Institute. "Part D, Protista 3". Treatise on Invertebrate Paleontology.
  6. ^ Paleontological Institute. "Part E, Archaeocyatha". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  7. ^ Paleontological Institute. "Part E, Archaeocyatha (Revised)". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  8. ^ Paleontological Institute. "Part E, Porifera (Revised), vol. 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  9. ^ Paleontological Institute. "Part E, Porifera (Revised), vol. 3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  10. ^ Paleontological Institute. "Part E, Porifera (Revised), vol. 4-5". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  11. ^ Paleontological Institute. "Part F, Coelenterata". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  12. ^ Paleontological Institute. "Part F, Coelenterata, Supplement 1, vol. 1 & 2". Treatise on Invertebrate Paleontology. Retrieved 5 December 2013.{{cite web}}: CS1 maint: url-status (link)
  13. ^ Paleontological Institute. "Part G, Bryozoa". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  14. ^ Paleontological Institute. "Part G, Bryozoa (Revised), vol. 1". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  15. ^ Paleontological Institute. "Part H, Brachiopoda, vol. 1 & 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  16. ^ Paleontological Institute. "Part H, Brachiopoda (Revised), vol. 1". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  17. ^ Paleontological Institute. "Part H, Brachiopoda (Revised), vol. 2 & 3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  18. ^ Paleontological Institute. "Part H, Brachiopoda (Revised), vol. 4". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  19. ^ Paleontological Institute. "Part H, Brachiopoda (Revised), vol. 5". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  20. ^ Paleontological Institute. "Part H, Brachiopoda (Revised), vol. 6". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  21. ^ Paleontological Institute. "Part I, Mollusca 1". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  22. ^ Paleontological Institute. "Part K, Mollusca 3". Treatise on Invertebrate Paleontology.
  23. ^ Paleontological Institute. "Part L, Mollusca 4". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  24. ^ Paleontological Institute. "Part L, Mollusca 4 (Revised), vol. 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  25. ^ Paleontological Institute. "Part L, Mollusca 4 (Revised), vol. 4". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  26. ^ Paleontological Institute. "Part N, Mollusca 6, vol. 1 & 2". Treatise on Invertebrate Paleontology.
  27. ^ Paleontological Institute. "Part N, Mollusca 6, vol. 3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  28. ^ Paleontological Institute. "Part O, Arthropoda 1". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  29. ^ Paleontological Institute. "Part O, Arthropoda 1 (Revised), vol. 1". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  30. ^ Paleontological Institute. "Part P, Arthropoda 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  31. ^ Paleontological Institute. "Part Q, Arthropoda 3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  32. ^ Paleontological Institute. "Part R, Arthropoda 4, vol. 1 & 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  33. ^ Paleontological Institute. "Part R, Arthropoda 4, vol. 3 & 4". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  34. ^ Paleontological Institute. "Part S, Echinodermata 1, vol. 1 & 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  35. ^ Paleontological Institute. "Part 2, Echinodermata 2, vol. 1-3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  36. ^ Paleontological Institute. "Part T, Echinodermata 2 (Revised), vol. 3". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  37. ^ Paleontological Institute. "Part U, Echinodermata 3, vol. 1 & 2". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  38. ^ Paleontological Institute. "Part V, Graptolithina". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  39. ^ Paleontological Institute. "Part V, Graptolithina (Revised)". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  40. ^ Paleontological Institute. "Part W, Miscellanea". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  41. ^ Paleontological Institute. "Part W, Miscellanea (Revised)". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)
  42. ^ Paleontological Institute. "Part W, Miscellanea, Supplement 2: Conodonta". Treatise on Invertebrate Paleontology.{{cite web}}: CS1 maint: url-status (link)

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