Готові списки джерел за темами / History of geology and palaeontology

Добірка наукової літератури з теми "History of geology and palaeontology"

Автор: Grafiati
Опубліковано: 6 вересня 2023

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Статті в журналах з теми "History of geology and palaeontology"

1

Clarkson, E. N. K. "A brief history of Scottish palaeontology 1834–1984." Scottish Journal of Geology 21, no. 4 (June 1985): 389–406. http://dx.doi.org/10.1144/sjg21040389.

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2

Mcnamara, Kenneth, and Frances Dodds. "The Early History of Palaeontology in Western Australia: 1791-1899." Earth Sciences History 5, no. 1 (January 1, 1986): 24–38. http://dx.doi.org/10.17704/eshi.5.1.t85384660311h176.

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The exploration of the coast of Western Australia by English and French explorers in the late eighteenth and early nineteenth centuries led to the first recorded discoveries of fossiliferous rocks in Western Australia. The first forty years of exploration and discovery of fossil sites in the State was restricted entirely to the coast of the Continent. Following the establishment of permanent settlements in the 1820s the first of the inland fossil localities were located in the 1830s, north of Albany, and north of Perth. As new land was surveyed; particularly north of Perth, principally by the Gregory brothers in the 1840s and 1850s, Palaeozoic rocks were discovered in the Perth and Carnarvon Basins. F.T. Gregory in particular developed a keen interest in the geology of the State to such an extent that he was able, at a meeting of the Geological Society of London in 1861, to present not only a geological map of part of the State, but also a suite of fossils which showed the existence of Permian and Hesozoic strata. The entire history of nineteenth century palaeontology in Western Australia was one of discovery and collection of specimens. These were studied initially by overseas naturalists, but latterly, in the 1890s by Etheridge at The Australian Museum in Sydney. Sufficient specimens had been collected and described by the turn of the century that the basic outline of the Phanerozoic geology of the sedimentary basins was reasonably well known.
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3

Polly, P. David, Jussi T. Eronen, Marianne Fred, Gregory P. Dietl, Volker Mosbrugger, Christoph Scheidegger, David C. Frank, John Damuth, Nils C. Stenseth, and Mikael Fortelius. "History matters: ecometrics and integrative climate change biology." Proceedings of the Royal Society B: Biological Sciences 278, no. 1709 (January 12, 2011): 1131–40. http://dx.doi.org/10.1098/rspb.2010.2233.

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Climate change research is increasingly focusing on the dynamics among species, ecosystems and climates. Better data about the historical behaviours of these dynamics are urgently needed. Such data are already available from ecology, archaeology, palaeontology and geology, but their integration into climate change research is hampered by differences in their temporal and geographical scales. One productive way to unite data across scales is the study of functional morphological traits, which can form a common denominator for studying interactions between species and climate across taxa, across ecosystems, across space and through time—an approach we call ‘ecometrics’. The sampling methods that have become established in palaeontology to standardize over different scales can be synthesized with tools from community ecology and climate change biology to improve our understanding of the dynamics among species, ecosystems, climates and earth systems over time. Developing these approaches into an integrative climate change biology will help enrich our understanding of the changes our modern world is undergoing.
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4

Barnes, E. "The Bone Trail: generating enthusiasm for earth sciences in the classroom and museum." Geological Curator 8, no. 7 (July 2007): 321–23. http://dx.doi.org/10.55468/gc386.

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"The Bone Trail" is an exciting education project which was piloted in 2006. It was funded jointly by the British Society for the History of Science, Bolton Local Authority Secondary Strategy, and the Manchester Museum. Ateam of three educators - one academic historian of science (the author), and two science teachers (Peter Fowler and Alison Henning) - designed two full days of activities for Year 9 students on the history of comparative anatomy, geology, and palaeontology.
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5

Middlemiss, Frank A. "A brief history of Geology at Queen Mary." Proceedings of the Geologists' Association 108, no. 3 (January 1997): 165–70. http://dx.doi.org/10.1016/s0016-7878(97)80023-5.

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6

Howarth, Richard J. "The Role of Women in the History of Geology." Proceedings of the Geologists' Association 119, no. 3-4 (January 2008): 351–54. http://dx.doi.org/10.1016/s0016-7878(08)80311-2.

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7

HUANG, DIYING, ZHIJUN ZHANG, CHENYANG CAI, and TAIPING GAO. "Prof. Yong-Chong Hong: a Chinese pioneering palaeoentomologist." Palaeoentomology 2, no. 5 (October 31, 2019): 404–12. http://dx.doi.org/10.11646/palaeoentomology.2.5.1.

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Professor You-Chong Hong, a famous Chinese palaeoentomologist, was born in Nan’ao County, Shantou City, Guangdong Province on 5 November 1929 and passed away in Beijing on 4 July 2019. In 1953, Prof. Hong graduated from the Beijing College of Geology (China University of Geosciences, Beijing) and was assigned to the Laboratory of Ferrous Metal of the Department of Geology and Minerals of the Ministry of Geology. From 1957 to 1958, he worked in the Department of Stratigraphy and Palaeontology, Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences. He studied fossil mollusks and later fossil insects in the Soviet Academy of Sciences from 1958 to 1960 (Fig. 1). He returned to the Chinese Academy of Geological Sciences from 1960 to 1963; worked at the Tianjin Institute of Geology and Mineral Resources, Ministry of Geology and Minerals from 1963 to 1984; and worked at the Beijing Museum of Natural History after 1984.
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8

Bessudnova, Zoya. "Grigory (Gotthelf) Fischer Von Waldheim (1771-1853): Author of the First Scientific Works on Russian Geology and Palæontology." Earth Sciences History 32, no. 1 (January 1, 2013): 102–20. http://dx.doi.org/10.17704/eshi.32.1.n68416x30q1l4916.

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Sometimes called the 'Russian Cuvier', Grigory Fischer von Waldheim was born in 1771 in Waldheim near Freiberg in Saxony and graduated in 1792 from the Freiberg Mining Academy, where he studied under Werner and became friends with von Buch and von Humboldt. In Paris, he studied under Cuvier and the two became friends. In Russia, Fischer became Director of the Moscow University Natural History Museum (1804-1832), founder of the Moscow Society of Naturalists at Moscow University (1805), Corresponding Member (1805) and Honorary Member (1819) of the Imperial Academy of Sciences, and Professor (later President) of the Moscow Medical-Surgical Academy (1837), where he established its Natural History Museum. He gave systematic descriptions of materials in the Paris National Natural History Museum (1802-1803) and Moscow University's Natural History Museum (1805-1806). Using binomial nomenclature, he published the first scientific descriptions of the fossil fauna of Russia (1809) and the first descriptions of the fossil flora from around Moscow (1826) and the southwestern Urals (1840). He also wrote the first Russian monograph on geology and palaeontology (Oryctography of the Province of Moscow, 1830-1837). In effect, he founded palaeontology in Russia. His achievements were recognized during his lifetime and are remembered today in Germany and Russia, but are rather little known in the Anglophone world.
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9

Trewin, Nigel H. "History of research on the geology and palaeontology of the Rhynie area, Aberdeenshire, Scotland." Transactions of the Royal Society of Edinburgh: Earth Sciences 94, no. 4 (December 2003): 285–97. http://dx.doi.org/10.1017/s0263593300000699.

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ABSTRACTGeological and palaeontological research in the Rhynie area, Aberdeenshire, Scotland, has progressed in several stages. Following early surveys in the nineteenth century, Dr William Mackie mapped the western margin of the basin in 1910–1913, and discovered the plant-bearing chert. Following trenching of the chert in 1913, Kidston & Lang described the plant fossils between 1917 and 1921 and Scourfield, Hirst and Maulik the arthropods in the 1920s. Following a ‘dark age’ of some 30 years, Geoffrey Lyon awakened interest in the late 1950s. Trenching in 1963–1971 provided Lyon and his co-workers with new material, and resulted in finds of new plants and reinterpretations of earlier work. The next phase was initiated by Winfried Remy's discovery of gametophytes in material given to him by Lyon. Since 1980, the Münster school has continued to make exciting discoveries. Aberdeen University involvement began in 1987 with geochemical work confirming a hot spring origin for the chert. Drill cores taken in 1988 and 1997, and further trenching have allowed structural, sedimentological and stratigraphic reappraisals, and resulted in the discovery of a new biota in the Windyfield chert. Long-term collaborative international research continues to advance interpretation of this unique Early Devonian hot spring system, and the remarkably diverse freshwater and terrestrial biota of the cherts.
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10

ŞENGÖR, A. M. C. "EDUARD SUESS AND PALAEONTOLOGY: HIS ILLUSTRATIONS." Earth Sciences History 40, no. 2 (July 1, 2021): 461–502. http://dx.doi.org/10.17704/1944-6187-40.2.461.

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The very first scientific paper by the great Austrian geologist Eduard Suess (1831–1914), the dean of geologists internationally during his lifetime, treats the graptolites of Bohemia (the ‘Barrandian’). This paper and most of his subsequent papers on palaeontology are accompanied by superb drawings of his observations in which Suess took great care not to insert himself between Nature as he perceived it in the framework of the knowledge of his day and his readers. In his drawings, he exercised what the great German geologist Hans Cloos later called ‘the art of leaving out’. This meant that in the drawings, the parts not relevant to the discussion are left only in outline, whereas parts he wished to highlight are brought to the fore by careful shading; but even the parts left only in outline are not schematic, instead they are careful reconstructions true to Nature as much as the material allowed it. This characteristic of Suess’ illustrations is seen also in his later field sketches concerning stratigraphy and structural geology and also in his depiction of the large tectonic features of our globe representing a guide to his manner of thinking. His illustrations in his early palaeontological work foreshadowed the later global geologist’s approach to our planet (and the Moon!) as a whole.
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Дисертації з теми "History of geology and palaeontology"

1

Blaj, Teodora. "Late Eocene through Oligocene calcareous nannofossils from the paleo-equatorial Pacific Ocean – taxonomy, preservation history, biochronology and evolution." Doctoral thesis, Stockholm : Department of geology and geochemistry, Stockholm university, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-27600.

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2

Ratcliffe, Kenneth T. "Sedimentology, palaeontology and diagenesis of the Much Wenlock limestone formation." Thesis, Aston University, 1987. http://publications.aston.ac.uk/14369/.

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Lithofacies distribution indicates that the Much Wenlock Limestone Formation of England and South Wales was desposited on a shelf which was flat and gently subsiding in the north, but topographically variable in the south. Limestone deposition in the north began with 12m of alga-rich limestone, which formed an upward shoaling sequence. Deepening then led to deposition of calcareous silty mudstones on the northern shelf. The remainder of the formation in this area formed during a shelf-wide regression, culminating in the production of an E to W younging sandbody. Lithofacies distribution on the southern shelf was primarily controlled by local subsidence. Six bedded lithofacies are recognised which contain 14 brachiopod/bryozoan dominated assemblages, of which 11 are in situ and three consist of reworked fossils. Microfacies analysis is necessary to distinguish assemblages which reflect original communities from those which reflect sedimentary processes. Turbulence, substrate-type, ease of feeding and other organisms in the environment controlled faunal distribution. Reefs were built dominantly by corals, stromatoporoids, algae and crinoids. Coral/stromatoporoid (Type A) reefs are common, particularly on the northern shelf, where they formed in response to shallowing, ultimately growing in front of the advancing carbonate sandbody. Algae dominate Type B and Type C reefs, reflecting growth in areas of poor water circulation. Lithification of the formation began in the marine-phreatic environment with precipitation of aragonite and high Mg calcite, which was subsequently altered to turbid low Mg calcite. Younger clear spars post-date secondary void formation. The pre-compactional clear spars have features which resemble the products of meteoric water diagenesis, but freshwater did not enter the formation at this time. The pre-compactional spars were precipitated by waters forced from the surrounding silty mudstones at shallow burial depths. Late diagenetic products are stylolites, compaction fractures and burial cements.
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3

Vandome, Robin Cheyne. "Intellectual transformations in American geology, palaeontology and anthropology, 1850-1900." Thesis, University of Cambridge, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.608533.

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4

Pitchford, Andrew John. "The stratigraphy, palaeontology, and palaeoecology of the Campanian Chalk of Norfolk." Thesis, University of Liverpool, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.291739.

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5

Smith, Michael Paul. "Ibexian-Whiterockian (Ordovician) conodont palaeontology of east and eastern north Greenland." Thesis, University of Nottingham, 1985. http://eprints.nottingham.ac.uk/14311/.

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Samples collected from mid-Ibexian (mid-Tremadoc) to late Whiterockian (Llandeilo) of East and eastern North Greenland have yielded a total of 9,725 identifiable conodont clements. The conodonts are referred to 54 multi-element genera and 115 species, new taxa include three genera (Macheticodus, Wandelia and Wcbcrina) and nine species (Eucharodus apion, Macheticodus lekiskus, Multioistodus? celox, Pteracontiodus armillatus, Scalpellodus? narvhalensis, Sibiriodus? kalalekus, Wandelia fuscina, Weberina candidisphaera and Weberina guyi). The faunas are coniform-dominated and generally similar to shallow water, Midcontinent Province faunas found in North America. Some degree of endemicity is indicated by the presence of species found only in the eastern Canadian Arctic Islands and Greenland. The conodonts are referred to ten biozones, of which three zones in the Ibexian are newly named (the Loxodus bransoni, Glyptoconus quadraplicatus and Oepikodus communis Zones) as are three Ibexian sub-zones (the Acodus deltatus,?Reutterodus andinus and Protoprioniodus aranda). These are all based on the previous, informal faunal divisions established in North America. In East Greenland, the oldest faunas recovered, from the base of the Cape Weber Formation on Ella Ø, are referred to the L.bransoni Zone (mid-Ibexian). Both upper and lower boundaries are, however, diachronous and on Albert Heim Bjerge, 150km to the north, the base of the formation contains conodonts of the younger G.quadraplicatus Zone. On Ella Ø, the lbexian-Whiterockian boundary occurs within the lower part of the Narwhale Sound Formation and the youngest conodonts recovered are referable to the Histiodella altifrons Zone (early Whiterockian). The youngest Ordovician conodonts recovered from East Greenland are from the Heim Bjerge Formation, directly underlying Devonian conglomerates, on C.H.Ostenfeld Nunatak; these faunas contain taxa of the Polyplacognathus sweeti Zone (late Whiterockian). In eastern North Greenland, the Wandel Valley Formation unconformably overlies Cambrian carbonates, and conodonts recovered from the base probably belong to the O.communis Zone (late lbexian). The Ibexian-Whiterockian boundary lies at or just above the lower boundary of the Upper Member and the top of the formation contains taxa referable to the Polyplacognathus friendsvillensis Zone (late Whiterockian). Contouring of the colour alteration indices (CAl) in North Greenland indicates that the isotherms are parallel to the margin of the Hazen Trough; to the east, in Kronprins Christian Land, they swing around to become parallel to the Caledonian front. Fused clusters recovered from the Cape Weber and Heim Bjerge Formations are amongst the oldest euconodont assemblages recorded. They are principally of coniform species and suggest a grasping function analogous to that of chaetognath spines.
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Martill, David Michael. "Studies on the vertebrate palaeontology of the Oxford Clay (Jurassic) of England." Thesis, University of Leicester, 1985. http://hdl.handle.net/2381/8441.

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7

Pether, John. "The sedimentology, palaeontology and stratigraphy of coastal-plain deposits at Hondeklip Bay, Namaqualand, South Africa." Master's thesis, University of Cape Town, 1994. http://hdl.handle.net/11427/22469.

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Bibliography: pages 295-307.
The exposures in diamond mines on the Namaqualand west coast of South Africa provide a rare opportunity to examine a record that is normally inaccessible beneath a thick cover of aeolian sands. This study presents the main results of fieldwork in mine excavations on the farms Hondeklip and Avontuur-A, near Hondeklip Bay. Sections in the deposits were described in detail and the vertebrate and invertebrate faunas were sampled. The buried topography of the gneiss bedrock, obtained by prospecting, is complex, with the main feature consisting of a coast-parallel ridge flanking a wide palaeochannel on its landward side. Advanced kaolinitic weathering affected both the bedrock and a diamondiferous, basal kaolinitic sediment patchily preserved in the channel. The incision of the channel is related to the Oligocene regression and the basal kaolinitic sediment is interpreted as a fluvial arkose deposited in the channel. Both the bedrock and the deposit in the channel were then kaolinized during humid climatic conditions in the late Oligocene and early Miocene. Weathering-profile silcrete also developed in the basal kaolinitic sediment. It is tentatively proposed that this weathering period may be represented in the Namib Desert by the thick laterite capping Eocene sediments at Kakaoberg. Subsequently, the palaeochannel was exhumed and was ultimately filled by late Tertiary marine deposits. The marine deposits were laid down in shallowing-upwards sequences of the shore face environment. Two regressive, progradational packages (alloformations) are recognized. The older extends seawards from at least -50 m asl. and is the "45-50 m Complex" of Carrington and Kensley (1969), now called the 50 m Package. East of the channel, on the exposed coast, high-wave-energy storm-deposition in the lower shoreface dominates the preserved record. With lowering of sea-level, the bedrock ridge emerged to the seaward of the prograding palaeoshoreline, reduced the level of incident wave energy and profoundly influenced the development of sub-environments within the progradational regime. Ultimately, low-energy bay deposits filled the palaeochannel in the bedrock. On the basis of vertebrate evidence and correlation with global sea-level trends, the age of the 50 m Package is middle Pliocene. The upper facies of the 50 m Package (foreshore and upper shoreface) have been extensively removed by later subaerial erosion. The subsequent transgression truncated the seaward extent of the 50 m Package, reached ~30 m asl. and prograded seaward from that elevation. It is called the 30 m Package and combines the "29-34 m Beach" and "17-21 m Complex" of Carrington and Kensley (1969). A late Pliocene age is envisaged. The upper-shoreface facies of the 30 m Package is usually preserved, but may be disguised by pedogenesis. The diamondiferous marine gravels mined in the area are mainly lower-shoreface storm deposits and pre-existing transgressive lags and shelf deposits have generally been reworked during regression. Enigmatic, muddy and/or phosphatic units, previously called "E-stage," are patchily preserved in the base of the 50 m Package and are revealed to be distal storm deposits laid down in the transitional shoreface to offshore environment. They are part of the overlying regressive sequence, but may include a fragmentary , petrified, mixed, vertebrate remanie. Nevertheless, eroded remnants of older deposits must also occur in places.
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Sun, Weiguo. "Contributions to palaeontology and stratigraphic correlation of the late precambrian in China and Australia /." Title page, contents and summary only, 1985. http://web4.library.adelaide.edu.au/theses/09PH/09phs957.pdf.

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9

Pazio, Magdalena. "The late Ediacaran Agglutinated Foraminifera from Finnmark, Northern Norway." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-183994.

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Daley, Allison C. "The morphology and evolutionary significance of the anomalocaridids." Doctoral thesis, Uppsala universitet, Paleobiologi, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-114102.

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Approximately 600 to 500 million years ago, a major evolutionary radiation called the “Cambrian Explosion” gave rise to nearly all of the major animal phyla known today. This radiation is recorded by various fossil lagerstätten, such as the Burgess Shale in Canada, where soft-bodied animals are preserved in exquisite detail. Many Cambrian fossils are enigmatic forms that are morphologically dissimilar to their modern descendants, but which still provide valuable information when interpreted as stem-group taxa because they record the actual progression of evolution and give insight into the order of character acquisitions and homologies between living taxa. One such group of fossils is the anomalocaridids, large presumed predators that have had a complicated history of description. Their body has a trunk with a series of lateral lobes and associated gills, and a cephalic region with a pair of large frontal appendages, a circular mouth apparatus, stalked eyes and a cephalic carapace. Originally, two taxa were described from the Burgess Shale, Anomalocaris and Laggania, however data presented herein suggests that the diversity of the anomalocaridids was much higher. Newly collected fossil material revealed that a third Burgess Shale anomalocaridid, Hurdia, is known from whole-body specimens and study of its morphology has helped to clarify the morphology and systematics of the whole group. Hurdia is distinguished by having mouthparts with extra rows of teeth, a unique frontal appendage, and a large frontal carapace. Two species, Hurdia victoria and Hurdia triangulata were distinguished based on morphometric shape analysis of the frontal carapace. A phylogenetic analysis placed the anomalocaridids in the stem lineage to the euarthropods, and examination of Hurdia’s well-preserved gills confirm the homology of this structure with the outer branches of limbs in upper stem-group arthropods. This homology supports the theory that the Cambrian biramous limb formed by the fusion of a uniramous walking limb with a lateral lobe structure bearing gill blades. In this context, new evidence is present on the closely allied taxon Opabinia, suggesting that it had lobopod walking limbs and a lateral lobe structure with attached Hurdia-like gills. The diversity of the anomalocaridids at the Burgess Shale is further increased by two additional taxa known from isolated frontal appendages. Amplectobelua stephenensis is the first occurrence of this genus outside of the Chengjiang fauna in China, but Caryosyntrips serratus is an appendage unique to the Burgess Shale. To gain a better understanding of global distribution, a possible anomalocaridid is also described from the Sirius Passet biota in North Greenland. Tamisiocaris borealis is known from a single appendage, which is similar to Anomalocaris but unsegmented, suggesting this taxon belongs to the arthropod stem-lineage, perhaps in the anomalocaridid clade. Thus, the anomalocaridids are a widely distributed and highly diverse group of large Cambrian presumed predators, which provide important information relevant to the evolution of the arthropods.
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Книги з теми "History of geology and palaeontology"

1

Farrand, William R. Depositional history of Franchthi Cave: Stratigraphy, sedimentology, and chronology. Bloomington: Indiana University Press, 2000.

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2

Johnson, Kirk R. Prehistoric journey: A history of life on earth. Denver: Denver Museum of Natural History, 1995.

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3

K, Stucky Richard, ed. Prehistoric journey: A history of life on earth. Boulder, Colorado: Roberts Rinehart Publishers, 1995.

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4

Keith, Stucky Richard, ed. Prehistoric journey: A history of life on Earth. Golden, Colo: Fulcrum Pub., 2006.

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5

H, Walliser Otto, and Ziegler Willi, eds. Contributions to Devonian palaeontology and stratigraphy. Frankfurt am Main: Senckenbergische Naturforschende Gesellschaft, 1989.

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6

Bromley, Richard G. Trace fossils: Biology and taphonomy. London: Chapman & Hall, 1994.

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7

S, Peel John, ed. North Greenland Lower Palaeozoic palaeontology and stratigraphy: Short contributions. Copenhagen: Grønlands geologiske undersøgelse, 1986.

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8

1933-, Hallam A., and Naturvetenskapliga forskningsrådet (Sweden), eds. Historical geology and palaeontology: Report to the Research Council. Stockholm: Swedish Natural Science Research Council, 1989.

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9

H, Ludbrook N., and Lindsay J. M. 1929-, eds. Stratigraphy, palaeontology, malacology: Papers in honour of Dr. Nell Ludbrook. [Parkside]: Dept. Mines and Energy, South Australia, 1985.

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10

S, Peel John, ed. Palaeontology, stratigraphy, and environmental setting of Middle Cambrian outer shelf deposits, north Greenland. Copenhagen: Grønlands geologiske undersøgelse, 1994.

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Частини книг з теми "History of geology and palaeontology"

1

Chapple, J. A. V. "Palaeontology, Geology, Zoology, Biology." In Science and Literature in the Nineteenth Century, 58–98. London: Macmillan Education UK, 1986. http://dx.doi.org/10.1007/978-1-349-18470-5_3.

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Ghorbani, Mansour. "History of Mining." In Springer Geology, 65–78. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5625-0_3.

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Prost, Gary L., and Benjamin P. Prost. "Earth History." In The Geology Companion, 85–116. Boca Raton : CRC Press, 2017.: CRC Press, 2017. http://dx.doi.org/10.1201/9781315152929-6.

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Murdmaa, Ivar, Elena Ivanova, and Dmitrii Borisov. "History of the Ioffe Drift." In Springer Geology, 161–82. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-82871-4_10.

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Ponce, Juan Federico, and Marilén Fernández. "Geology." In Climatic and Environmental History of Isla de los Estados, Argentina, 35–43. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-4363-2_4.

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Guevara, David Nelson Federico. "History of Gold in Tierra del Fuego." In Springer Geology, 97–154. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-60683-1_8.

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Rothenburg, Daniel. "History, Geography, and Geology." In Irrigation, Salinity, and Rural Communities in Australia's Murray-Darling Basin, 1945–2020, 19–30. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-18451-2_2.

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Wu, C. J., G. L. Ye, J. R. Sheng, and J. H. Wang. "Depositional History and Geotechnical Properties of Shanghai Clays." In Springer Geology, 269–73. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31671-5_49.

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Etter, Walter. "Conrad Gessner and the Early History of Palaeontology." In Conrad Gessner, edited by Urs Leu and Peter Opitz, 129–44. Berlin, Boston: De Gruyter, 2019. http://dx.doi.org/10.1515/9783110499056-008.

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Motuza, Gediminas. "Research History and the Sources of Information." In Regional Geology Reviews, 3–11. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-96855-7_2.

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Тези доповідей конференцій з теми "History of geology and palaeontology"

1

Matveev, Ivan, Gleb Shishaev, Grachik Eremyan, Vasily Demyanov, Oksana Popova, Sergey Kaygorodov, Boris Belozerov, Iuliia Uzhegova, Dmitry Konoshonkin, and Mikhail Korovin. "Geology Driven History Matching." In SPE Russian Petroleum Technology Conference. Society of Petroleum Engineers, 2019. http://dx.doi.org/10.2118/196881-ms.

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Matveev, Ivan, Gleb Shishaev, Grachik Eremyan, Vasily Demyanov, Oksana Popova, Sergey Kaygorodov, Boris Belozerov, Iuliia Uzhegova, Dmitry Konoshonkin, and Mikhail Korovin. "Geology Driven History Matching (Russian)." In SPE Russian Petroleum Technology Conference. Society of Petroleum Engineers, 2019. http://dx.doi.org/10.2118/196881-ru.

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3

Yajima, Michiko, and Toshihiro Yamada. "MODENIZING STENO’S PRODROMUS(1669): STENONIAN HERITAGE IN THE HISTORY OF EVOLUTIONARY PALAEONTOLOGY IN JAPAN." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336327.

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Matveev, I., G. Shishaev, G. Eremyan, D. Konoshonkin, V. Demyanov, and S. Kaygorodov. "Geology Realism Control in Automated History Matching." In ECMOR XVII. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202035243.

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Crigo, D., C. Daturi, and C. Rizzi. "Tunisia Offshore a Basin Modelling Assisted Exploration History." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406032.

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Foky, Trent. "Unraveling the geomorphic history of Blacktail Deer Creek." In Proceedings of the Keck Geology Consortium. Keck Geology Consortium, 2020. http://dx.doi.org/10.18277/akrsg.2020.33.14.

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Grabowski, G. J. "Stratigraphy and Depositional History of the Marib-Jawf Basin, Yemen." In Fourth Arabian Plate Geology Workshop. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142784.

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Aubele, Jayne C., and Larry S. Crumpler. "21ST CENTURY NATURAL HISTORY: PLANETARY GEOLOGY IN MUSEUMS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286924.

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Whitlock, Cathy. "CLIMATE AND GEOLOGY HAVE SHAPED YELLOWSTONE’S ECOLOGICAL HISTORY." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-378349.

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Cerro, R., B. Parlov, and J. Samarzija. "Croatian Offshore Adriatic - A Case History of Gas Effects Combination." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406035.

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Звіти організацій з теми "History of geology and palaeontology"

1

Josenhans, H. W., and J. Zevenhuizen. Quaternary geology I, Labrador sea, Quaternary history. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127156.

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Klassen, R. A. Quaternary geology and glacial history of Bylot Island, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/183984.

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3

Bednarski, J. M. Surficial geology and sea level history of Bathurst Island, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207432.

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Kaszycki, C. A., L. A. Dredge, and H. Groom. Surficial geology and glacial history, Lynn Lake - Leaf Rapids area, Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225935.

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Bell, T., and D. A. Hodgson. Quaternary geology and glacial history of Fosheim Peninsula, Ellesmere Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211957.

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Reger, R. D., and W. A. Petrik. Surficial geology and late Pleistocene history of the Anchor Point area, Alaska. Alaska Division of Geological & Geophysical Surveys, 1993. http://dx.doi.org/10.14509/1610.

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Kaszycki, C. A. Quaternary geology and glacial history of the Haliburton region, south central Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/208201.

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Meyer, J. M., and R. Leonardson. Geology of the Questa mining district--Volcanic, plutonic, tectonic, and hydrothermal history. New Mexico Bureau of Geology and Mineral Resources, 1997. http://dx.doi.org/10.58799/ofr-431.

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9

Dredge, L. A. Quaternary geology of northern Melville Peninsula, District of Franklin, Northwest Territories: surface deposits, glacial history, environmental geology, and till geochemistry. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205729.

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Richard, P. J. H. Late Wisconsinan and Holocene Vegetational History [Chapter 3: Quaternary Geology of the Canadian Shield]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127973.

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