Relevant bibliographies by topics / Bryozoa, Fossil

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Bryozoa, Fossil'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Bryozoa, Fossil.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Bryozoa, Fossil"

1

O'Dea, Aaron, and Beth Okamura. "Life history and environmental inference through retrospective morphometric analysis of bryozoans: a preliminary study." Journal of the Marine Biological Association of the United Kingdom 80, no. 6 (December 2000): 1127–28. http://dx.doi.org/10.1017/s0025315400003210.

Full text
Abstract:
A preliminary comparative analysis of colony growth and zooid size in the perennial bryozoan Flustra foliacea (Bryozoa: Cheilostomatida) reveals reduced colony growth in the Bay of Fundy relative to growth in the Menai Straits and the Skagerrak, while seasonal fluctuations in zooid size are in synchrony with temperature regimes. Such retrospective morphometric analyses may allow inferences of primary productivity and thermal regimes and provide insights into the life histories of both Recent and fossil bryozoans.
APA, Harvard, Vancouver, ISO, and other styles
2

Pagès-Escolà, M., PE Bock, DP Gordon, S. Wilson, C. Linares, B. Hereu, and MJ Costello. "Progress in the discovery of extant and fossil bryozoans." Marine Ecology Progress Series 635 (February 6, 2020): 71–79. http://dx.doi.org/10.3354/meps13201.

Full text
Abstract:
The number of species that exist on Earth has been an intriguing question in ecology and evolution. For marine species, previous works have analysed trends in the discovery of extant species, without comparison to the fossil record. Here, we compared the rate of description between extant and fossil species of the same group of marine invertebrates, Bryozoa. There are nearly 3 times as many described fossil species as there are extant species. This indicates that current biodiversity represents only a small proportion of Earth’s past biodiversity, at least for Bryozoa. Despite these differences, our results showed similar trends in the description of new species between extant and fossil groups. There has been an increase in taxonomic effort during the past century, characterized by an increase in the number of taxonomists, but no change in their relative productivity (i.e. similar proportions of authors described most species). The 20th century had the most species described per author, reflecting increased effort in exploration and technological developments. Despite this progress, future projections in the discovery of bryozoan species predict that around 10 and 20% more fossil and extant species than named species, respectively, will be discovered by 2100, representing 2430 and 1350 more fossil and extant species, respectively. This highlights the continued need for both new species descriptions and taxonomic revisions, as well as ecological and biogeographical research, to better understand the biodiversity of Bryozoa.
APA, Harvard, Vancouver, ISO, and other styles
3

GORDON, DENNIS P., and PHILIP E. BOCK. "Phylum Bryozoa Ehrenberg, 1831 in the first twenty years of Zootaxa." Zootaxa 4979, no. 1 (May 28, 2021): 236–39. http://dx.doi.org/10.11646/zootaxa.4979.1.27.

Full text
Abstract:
This short account is an invited contribution to the Zootaxa special volume ‘Twenty years of Zootaxa.’ Zootaxa was first published on 28 May 2001. Between this date and December 2020, 116 papers were published in Zootaxa that mention Bryozoa, comprising mostly descriptions of new species and higher taxa, but also including molecular sequencing (e.g. Fehlauer-Ale et al. 2011; Taylor et al. 2011; Franjevic et al. 2015), invasive-species research (e.g. Ryland et al. 2014; Vieira et al. 2014), checklists (e.g. Vieira et al. 2008), classification (e.g. Bock & Gordon 2013), bryozoans as associates of other organisms (e.g. Rudman 2007; Chatterjee & Dovgal 2020; Chatterjee et al. 2020), metazoan phylogeny (e.g. Giribet et al. 2013), biographies of historical figures who worked on bryozoans (e.g. Calder & Brinkmann-Voss 2011; Calder 2015) and a catalogue of the fossil invertebrate taxa described by William Gabb (including 67 bryozoan species) (Groves & Squires 2018). Of the 116 papers, 15 (13%) were open-access.
APA, Harvard, Vancouver, ISO, and other styles
4

Kopperud, Bjørn Tore, Scott Lidgard, and Lee Hsiang Liow. "Text-mined fossil biodiversity dynamics using machine learning." Proceedings of the Royal Society B: Biological Sciences 286, no. 1901 (April 24, 2019): 20190022. http://dx.doi.org/10.1098/rspb.2019.0022.

Full text
Abstract:
Documented occurrences of fossil taxa are the empirical foundation for understanding large-scale biodiversity changes and evolutionary dynamics in deep time. The fossil record contains vast amounts of understudied taxa. Yet the compilation of huge volumes of data remains a labour-intensive impediment to a more complete understanding of Earth's biodiversity history. Even so, many occurrence records of species and genera in these taxa can be uncovered in the palaeontological literature. Here, we extract observations of fossils and their inferred ages from unstructured text in books and scientific articles using machine-learning approaches. We use Bryozoa, a group of marine invertebrates with a rich fossil record, as a case study. Building on recent advances in computational linguistics, we develop a pipeline to recognize taxonomic names and geologic time intervals in published literature and use supervised learning to machine-read whether the species in question occurred in a given age interval. Intermediate machine error rates appear comparable to human error rates in a simple trial, and resulting genus richness curves capture the main features of published fossil diversity studies of bryozoans. We believe our automated pipeline, that greatly reduced the time required to compile our dataset, can help others compile similar data for other taxa.
APA, Harvard, Vancouver, ISO, and other styles
5

Zágoršek, Kamil, Sorin Filipescu, and Katarína Holcová. "New Middle Miocene Bryozoa from Gârbova de Sus (Romania) and their relationship to the sedimentary environment." Geologica Carpathica 61, no. 6 (December 1, 2010): 495–512. http://dx.doi.org/10.2478/v10096-010-0031-2.

Full text
Abstract:
New Middle Miocene Bryozoa from Gârbova de Sus (Romania) and their relationship to the sedimentary environmentThe section of Gârbova de Sus contains diverse fossil groups and rich bryozoan assemblages, with 77 species altogether. Several taxa have been recognized as very important in the assemblage and two new taxa are described in detail:Poricella garbovensissp. nov. andTherenia transylvanicasp. nov. Foraminifera and calcareous nannofossil assemblages were used for biostratigraphic and paleoenvironmental interpretations. On the basis of sedimentological features and micropaleontological data, the sequence of paleoenvironments can be subdivided into two intervals indicating slightly different climatic conditions.
APA, Harvard, Vancouver, ISO, and other styles
6

Taylor, Paul D., Björn Berning, and Mark A. Wilson. "Reinterpretation of the Cambrian ‘bryozoan’ Pywackia as an octocoral." Journal of Paleontology 87, no. 6 (November 2013): 984–90. http://dx.doi.org/10.1666/13-029.

Full text
Abstract:
Pywackia baileyi Landing in Landing et al., 2010, from the upper Cambrian Yudachica Member of Oaxaca State, southern Mexico, consists of small, phosphatic, proximally tapering cylindrical rods covered by shallow polygonal calices. The bryozoan-like morphology of this fossil prompted its interpretation as the first bryozoan known from the Cambrian. However, restudy of some of the original material, employing scanning electron microscopy for the first time, questions the assignment of Pywackia to the Bryozoa. Striking similarities between Pywackia and the modern pennatulacean octocoral Lituaria lead to an alternative hypothesis interpreting Pywackia an early fossil octocoral. While Pywackia is probably not a true pennatulacean, a group with a definitive fossil record stretching back only to the Late Cretaceous, it can be envisaged as having had a similar skeletal structure and ecology to Lituaria, the rods representing mineralized axes of tiny colonies that lived with their proximal ends buried in the sediment and distal ends covered by feeding polyps. Landing et al. (2010) considered the phosphatic composition of Pywackia specimens to be the result of diagenetic replacement, but the evidence is equivocal. If Pywackia had a primary phosphatic skeleton, this would support the hypothesized existence of phosphatic biomineralization early in the evolutionary history of Cnidaria, as well as providing further evidence that Pywackia is not a bryozoan.
APA, Harvard, Vancouver, ISO, and other styles
7

Bock, Philip E., and Patricia L. Cook. "First fossil finds of some Australian Bryozoa (Cheilostomata)." Alcheringa: An Australasian Journal of Palaeontology 25, no. 4 (January 2001): 407–24. http://dx.doi.org/10.1080/03115510108619231.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Lidgard, Scott, Frank K. McKinney, and Paul D. Taylor. "Competition, clade replacement, and a history of cyclostome and cheilostome bryozoan diversity." Paleobiology 19, no. 3 (1993): 352–71. http://dx.doi.org/10.1017/s0094837300000324.

Full text
Abstract:
One of the striking yet scarcely documented episodes of clade replacement in the post-Paleozoic fossil record is the decline of cyclostome Bryozoa and the corresponding, rapid diversification of cheilostome Bryozoa. These clades are closely associated morphologically and phylogenetically, and their ecological similarities have previously led to the inference that competition was a primary cause of the overt pattern of replacement. Alternatively, previous compilations of bryozoan families and genera have implied that extinctions at the Cretaceous/Tertiary boundary differentially affected cyclostomes, and thus were also an important factor in the transition.We first evaluated the ecological context for competition between the two clades, then updated and reexamined the history of absolute family diversity for bryozoans in consecutive geologic stages from Jurassic to Recent. The resulting trends echo the patterns shown in earlier family level compilations, but indicate a slight shift in the frequency of cheilostome family originations from Late Cretaceous to early Paleogene. The relative fall in cyclostome family diversity at the Cretaceous/Tertiary boundary is significantly less than shown in earlier genus level compilations. We then assessed these various compilations of absolute diversity by analyzing species counts and percentages in 728 fossil assemblages, primarily from North America and Europe, over the same time interval. Cyclostome species overwhelmingly dominate assemblages from Jurassic through Cenomanian, then decline significantly in average percentage dominance through the Campanian. Cheilostomes are predominant in Campanian and later assemblages. Cyclostome species percentages do decrease overall through the Tertiary, but this decrease is small and non-uniform, varying around 30%, with a sharp drop in the Late Neogene. Our within-assemblage results indicate that as cheilostomes radiate, their mean species diversity, maximum diversity, and variance all increase, thereby accounting for much of the decline in average percentage of cyclostomes within assemblages. While this result does not exclude a role for competition, an hypothesis of relative decline in cyclostome species richness based on competitive extinction alone seems unlikely. Further, despite decreases in absolute species counts following end-Cretaceous extinctions, within-assemblage percentages of cheilostome or cyclostome species show only slight change relative to one another. Comparison of these and earlier diversity compilations indicates that the dynamics of bryozoan clade replacement may be perceived differently at different ecologic scales or taxonomic ranks.
APA, Harvard, Vancouver, ISO, and other styles
9

GORDON, DENNIS P., KJETIL L. VOJE, and PAUL D. TAYLOR. "Living and fossil Steginoporellidae (Bryozoa: Cheilostomata) from New Zealand." Zootaxa 4350, no. 2 (November 17, 2017): 345. http://dx.doi.org/10.11646/zootaxa.4350.2.9.

Full text
Abstract:
The cheilostome bryozoan family Steginoporellidae in New Zealand comprises seven living species of Steginoporella. Three of these are new to science—Steginoporella discors n. sp., Steginoporella lineata n. sp. and Steginoporella modesta n. sp.—and one (Steginoporella magnifica) additionally occurs as a Plio-Pleistocene fossil. A new Early Pleistocene fossil species, Steginoporella tiara n. sp., is also recognised. The living species exhibit the full range of colonial morphologies known for the genus, and two of the new deep-shelf taxa described herein have the smallest known colonies, both linear, not exceeding 5 mm in width and 22 mm in length. One species has a recorded depth range down to 615 m, apparently the deepest known for the genus. Zooidal proportions vary, with a length:width ratio in the seven living species ranging from 1.31 to 1.81, exceeded only by that in the new fossil taxon, which has very elongate zooids. Notwithstanding the conspicuous differences in colonial and zooidal morphology, four of the living species appear to be closely related, sharing distinctive reticulation of opercular sclerites, a similar morphology of the median process and no B-zooid morphs. Only one New Zealand taxon has B-zooids. Biogeographically, all the species except S. magnifica (also known from Tonga) are nominally endemic, but it is possible that some of the deeper-water taxa may eventually be found outside the boundary of the New Zealand Exclusive Economic Zone. The operculum in Steginoporella species is initially a single thin layer continuous with the membranous frontal wall, becoming two-layered when fully functioning in feeding zooids and mandibulate B-zooids.
APA, Harvard, Vancouver, ISO, and other styles
10

GROVES, LINDSEY T., and RICHARD L. SQUIRES. "Annotated Catalog of the Fossil Invertebrates Described by, and Named for, William More Gabb (1839–1878)." Zootaxa 4534, no. 1 (December 21, 2018): 1. http://dx.doi.org/10.11646/zootaxa.4534.1.1.

Full text
Abstract:
William More Gabb [1839–1878] described 1163 fossil invertebrate taxa: Protozoa [1 species], Porifera [1 genus, 2 species], Cnidaria [12 species], Bryozoa (with G.H. Horn) [1 family, 8 genera, 67 species], Brachiopoda [15 species], Annelida [7 species], Mollusca [Bivalvia: 15 genera, 2 subgenera, 412 species; Gastropoda: 1 family, 2 subfamilies, 42 genera, 8 subgenera, 489 species; Scaphopoda: 10 species; Cephalopoda: 1 family, 3 genera, 51 species], Arthropoda [Crustacea: 2 species; Cirripedia 1 species], and Echinodermata [11 species]. Listed herein are all fossil taxa named by Gabb, type localities, institutional depository, and remarks concerning current taxonomic status, when known. An annotated list of Gabb’s fossil references is also included. Also listed herein are 134 fossil invertebrate taxa and 33 living mollusk taxa named for him.
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Bryozoa, Fossil"

1

Schmidt, Rolf. "Eocene bryozoa of the St Vincent Basin, South Australia - taxonomy, biogeography and palaeoenvironments /." Title page, abstract and contents only, 2003. http://web4.library.adelaide.edu.au/theses/09PH/09phs3491.pdf.

Full text
Abstract:
Thesis (Ph.D.)--University of Adelaide, School of Earth and Environmental Sciences, Discipline of Geology and Geophysics, 2003?
Includes Publication list by the author as appendix A. "July 2003." Includes bibliographical references (leaves 308-324).
APA, Harvard, Vancouver, ISO, and other styles
2

Knowles, Tanya. "Fossil cheilostome Bryozoa of the mid-Pliocene North Atlantic and the interference of environmental regimes." Thesis, University of Reading, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.501324.

Full text
Abstract:
The mid-Pliocene warm period (3.29-2.97 Ma) was a time broadly characterised by global warmth and high sea levels. It represents the last time in Earth history when the level of atmospheric CO2 was similar to today (~ 380 ppm) and as such, it may provide a model for future global warming. The Mean Annual Range of Temperature (MART) experienced by a bryozoan colony can be estimated utilising the inverse relationship between zooid size in cheilostome bryozoans and water temperature at the time of budding (O'Dea and Okamura, 2000a). In this study the technique is applied to Pliocene bryozoan material from the UK, US Coastal Plain, Florida and the Isthmus of Panama. Absolute temperatures have been reconstructed from stable isotopic analyses performed on bryozoans from a number of sites. This technique relies on the principle that the skeletal material is secreted in isotopic equilibrium with seawater. The lighter oxygen isotope, ¹⁶0, is preferentially incorporated into the skeleton during warmer temperatures therefore the ratio of ¹⁶0:¹⁸0 can act as a thermometer allowing temperature of the water at the time of skeleton formation to be inferred. Data from a range of latitudes provide information about shelf sea temperatures, and are found to be consistent with outputs from mid-Pliocene scenarios generated by numerical models of climate (General Circulation Models).
APA, Harvard, Vancouver, ISO, and other styles
3

Sogot, Caroline Elizabeth. "Hard substrate communities across the K-Pg boundary." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648377.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

O'Dea, Aaron. "Environmental inferences using recent and fossil bryozoans." Thesis, University of Bristol, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302204.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Sabri, Zakaria. "Révision systématique du genre Lichenopora Defrance, 1823 (Bryozoa, Cyclostomata)." Lyon 1, 1988. http://www.theses.fr/1988LYO11763.

Full text
Abstract:
Ce travail porte sur la revision systematique du genre lichenopora defrance 1823. On discute la validite du genre disporella considere comme synonyme de lichenopora; deux groupes ont ete identifie: les lichenopores discoides et les lichenopores lamellaires. On precise la repartition stratigraphique de quatre especes, la repartition paleogeographique du genre lichenopora du cretace jusqu'a l'actuel ainsi que les tendances evolutives et les liens phyletiques existants entre certaines especes
APA, Harvard, Vancouver, ISO, and other styles
6

Barbour, Susan Leigh. "Microstratigraphic Analysis of an Amalgamated Horizon in the Type Cincinnatian:Implications for Spatio-Temporal Resolution in the Fossil Record." University of Cincinnati / OhioLINK, 2002. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1030643781.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Holmquist, Emily Kristin. "Paleobiogeography of Devonian bryozoa in Laurussia." Diss., 2008.

Find full text
Abstract:
Thesis (M.S.)--Michigan State University. Dept. of Geological Sciences, 2008.
"Advisor, Dr. Robert L. Anstey"--Acknowledgements. "The purpose of this study is to delineate patterns of endemism in Devonian bryozoans in North America and Europe, and to suggest hypotheses for the development of biogeographic regions during the period"--Introd. Title from PDF t.p. (viewed on Aug. 4, 2009) Includes bibliographical references (p. 38-44). Also issued in print.
APA, Harvard, Vancouver, ISO, and other styles
8

Schmidt, Rolf 1972. "Eocene bryozoa of the St Vincent Basin, South Australia - taxonomy, biogeography and palaeoenvironments." 2003. http://web4.library.adelaide.edu.au/theses/09PH/09phs3491.pdf.

Full text
Abstract:
Includes Publication list by the author as appendix A. "July 2003." Includes bibliographical references (leaves 308-324) A stratigraphically detailed taxonomic study of fossil bryozoans within the Late Eocene sediments of the St Vincent Basin, South Australia. These taxa are compared with existing knowledge of fossil and recent faunas in Australia and other regions to enhance understanding of bryozoan evolution and dispersal. Bryozoan taxa and growth forms are used to interpret the palaeoenvironments of the Eocene Vincent Basin.
APA, Harvard, Vancouver, ISO, and other styles

Books on the topic "Bryozoa, Fossil"

1

Guha, Asit K. Bryozoan fauna of the Ariyalur Group (late Cretaceous), Tamil Nadu and Pondicherry, India. Calcutta: Geological Survey of India, 1996.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Gori͡unova, R. V. Morfologii͡a, sistema i filogenii͡a mshanok, otri͡ad Rhabdomesida. Moskva: "Nauka", 1985.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Conference, International Bryozoology Association. Proceedings of the 11th International Bryozoology Association Conference: Smithsonian Tropical Research Institute, Republic of Panama, January 26-31, 1998. Balboa, Republic of Panama: The Institute, 2000.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

International Conference on Bryozoa (6th 1983 Vienna Austria). Bryozoa: Ordovician to recent : papers presented at the 6th International Conference on Bryozoa, Vienna, Austria, 1983. Fredensborg: Olsen & Olsen, 1985.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

International, Conference on Bryozoa (9th 1992 School of Biological Sciences University of Wales Swansea). Biology and palaeobiology of Bryozoans: Proceedings of the 9th International Bryozoology Conference, School of Biological Sciences, University of Wales, Swansea, 1992. Fredensborg, Denmark: Olsen & Olsen, 1994.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Wellington), International Bryozoology Conference (10th 1995 Victoria University of. Bryozoans in space and time: Proceedings of the 10th International Bryozoology Conference, Victoria University of Wellington, Wellington, New Zealand, 1995. Wellington, N.Z: NIWA, 1996.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Gori͡unova, R. V. Filogenii͡a paleozoĭskikh mshanok. Moskva: Nauka, 1996.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

Snell, Joanna F. Bryozoa from the Much Wenlock Limestone (Silurian) Formation of the west Midlands and Welsh borderland. London: Palaeontographical Society, 2004.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

Hageman, Steven J. Effects of nonnormality on studies of morphological variation of a rhabdomesine bryozoan, Streblotrypa (Streblascopora) prisca (Gabb and Horn). Lawrence, Kan: University of Kansas, 1993.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Guha, Asit K. Fossil Thalamoporella (Bryozoa) from the Tertiary sequences of western Kachchh, Gujarat, India. Los Angeles, Calif: Hancock Institute for Marine Studies, University of Southern California, 2004.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Bryozoa, Fossil"

1

Scholz, Joachim, and George S. Levit. "Bryozoan Morphoprocesses." In Fossil and Recent Biofilms, 181–95. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-017-0193-8_11.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Yarinpil, Ariunchimeg. "Fossil Bryozoans in the Stratigraphy of Mongolia." In Springer Geology, 1027–30. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_195.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Mckinney, Frank K., Paul D. Taylor, and Scott Lidgard. "Predation on Bryozoans and its Reflection in the Fossil Record." In Predator—Prey Interactions in the Fossil Record, 239–61. Boston, MA: Springer US, 2003. http://dx.doi.org/10.1007/978-1-4615-0161-9_10.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

"2 Fossil record and evolution of Bryozoa." In Phylum Bryozoa, 11–56. De Gruyter, 2020. http://dx.doi.org/10.1515/9783110586312-002.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Taylor, P. D. "FOSSIL INVERTEBRATES | Bryozoans." In Encyclopedia of Geology, 310–20. Elsevier, 2005. http://dx.doi.org/10.1016/b0-12-369396-9/00022-8.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

"Competition Involving Bryozoans." In Fossil Behavior Compendium, 239. CRC Press, 2010. http://dx.doi.org/10.1201/9781439810590-c32.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

"*3Chapter 2 Competition Involving Bryozoans." In Fossil Behavior Compendium, 267–68. CRC Press, 2010. http://dx.doi.org/10.1201/9781439810590-37.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Bryozoa, Fossil"

1

Kopperud, Bjørn Tore, and Lee Hsiang Liow. "TEXT-MINING THE BRYOZOAN FOSSIL RECORD." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320408.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Bryozoa, Fossil' for particular source types:
Journal articles Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography