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Worm, Ole

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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP375.26
EISBN: 9781862396432
... Abstract Ole Worm, Professor of Medicine at Copenhagen University 1624–1654, collected natural objects and artefacts with a view to letting students learn through observation and the touch of real things. Among the objects were fossils. Through Worm’s correspondence from 1607 to 1654, his...
FIGURES
Series: GSA Special Papers
Published: 27 November 2018
DOI: 10.1130/2018.2535(06)
EISBN: 9780813795355
... ABSTRACT During the first half of the seventeenth century, the Danish polyhistor, Ole Worm (1588–1654), established a collection in Copenhagen, the Museum Wormianum, consisting of minerals, plants, animals, and man-made objects. The collection attracted visitors and was renowned throughout...
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Journal Article
Published: 01 March 2006
Journal of Paleontology (2006) 80 (2): 386–391.
... illustrating very well the important features of the material discussed, we have to thank our friend and colleague M. Kostak from the Charles University at Prague (Czech Republic). Work on isolated palaeoscolecidan material by OL was started under a habilitation grant of the German Science Foundation (DFG Le...
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Journal Article
Published: 01 April 2020
Earth Sciences History (2020) 39 (1): 219–220.
... and Learning in Seventeenth-Century Denmark,” Lisbet Tarp writes about Ole Worm’s Museum Wormianum, renowned throughout Europe for its collection of natural history objects. Tarp argues that although Worm made no significant new discoveries, himself, his museum played an important role in shaping...
Journal Article
Published: 01 January 2007
Journal of the Geological Society (2007) 164 (1): 227–242.
... filamentous microbes and diatoms, scattered coccoid microbes, fungal hyphae and spores, rare sponge spicules, and rare worm(?) tubes. The diatoms, coccoid microbes, and fungi were brought into the area with the detrital sediment. In ancient successions, distinction between sublacustrine, terrestrial, and some...
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Journal Article
Published: 25 February 2008
Geological Magazine (2008) 145 (3): 397–411.
..., by a worm-like symplectite, composed of 55 % Pl, 30 % Am and 15 % Opx. The worm-like symplectite fills spectacular embayments in Grt 1 (Fig. 5 ), suggesting it was the principal reactant. Schenk (1984) in the same context also describes coronas mostly formed by Pl + Opx around Grt 1 . The outer coarse...
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Journal Article
Journal: Geology
Published: 01 September 2006
Geology (2006) 34 (9): 793–796.
.... One of the most famous wunderkammer in Europe was that of Ole Worm, a Dane who ultimately sold his collection to the King of Denmark. Steno wrote ( Ziggelaar, 1997 , p. 179) that he saw the wunderkammer; in his travels throughout Europe he undoubtedly saw others that contributed to his development...
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Journal Article
Journal: Paleobiology
Published: 06 November 2015
Paleobiology (2016) 42 (1): 27–53.
... the potential effects of sample size on these analyses, the residuals of the regression line (OLS) are calculated by plotting the mean number of specimens per slab against total abundance; each bar on the residual plot represents a single taxon. These taxa were grouped...
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Journal Article
Published: 01 June 1973
Bulletin of the Seismological Society of America (1973) 63 (3): 1025–1039.
.... COUPLED TORSIONAL DYNAMIC ANALYSIS OF A MULTISTORY BUILDING 1029 -08 -04 04 Q8 -01 QI -I-01 L. f till ,H (a) fir, ~roRs -ol ol - -, o,4 08 -Ol 01 / (b) ii1~ rlJi )~TORS. -o/ ol \-o,J q.i -ge 04 / (c) H,, ,ill i1~ ii)~ i ~ s ck~w ro~s FIG. 4. (a) North-south second mode displacements. (b) East-west...
Journal Article
Published: 01 May 2003
Russ. Geol. Geophys. (2003) 44 (5): 417–431.
... µm in size, and interstitial segregations are usually <100 µm, with pure (free of microlites) glass spots measuring no more than 10–20 µm. Most xenoliths contain plagioclase in interstices, and only some of them, interstitial glass. Plagioclase often forms isometric and worm-like branching...
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Journal Article
Journal: Economic Geology
Published: 01 November 2015
Economic Geology (2015) 110 (7): 1879–1904.
... Total Mg # Sc V Cr Co Ni Cu Zn Rb Ba Th U Nb Ta Pb Sr Zr Hf Y La Ce Pr Nd Sm Gd Tb Dy Ho Er Tm Yb Lu 2013-6-36 Hornblendite 39°31′49″ 114°59′7″ Ol + Cpx + Opx + Am + Bio ± Pl No alteration 45.26 0.49 6.01 15.24 0.21 21.56 7.56 1.21 0.88 0.15 1.43...
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Journal Article
Published: 01 September 2020
Journal of Paleontology (2020) 94 (5): 881–886.
... Tuzoia and Isoxys , brachiopods, algae, and worm-like animals. Hurdiidae indet. was found in Bed B along with bivalved euarthropods Tuzoia , sponges, chancelloriids, and worm-like animals (Sun et al., 2020 ). On the basis of biostratigraphic correlation (e.g., Fletcher and Collins, 1998 , 2003...
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Journal Article
Published: 01 June 1995
Bulletin of the Seismological Society of America (1995) 85 (3): 747–754.
... pug '(g86I 'tunqI!IN pue _ H~ qsoo P:mtuofl '.E86I 'xno!II!d) pou.mlqo uooq oAeq sp:tooo:t .Rugunsl ugooo-doop sno!Ao~d OA~I£[U0 "s!tugunsl OA!S.tods!p Se olqe {(o9 '0 b/)d~ -qs!n~uBs!p £[xeoIO oxe sttuojoAe~ oso~ 'I oJn~t.d u! sp:tooo.l ogugg op.n ~oq:req oql ol lsexluoo uI "8 Pug V SlUOAOgq pole:tO...
Journal Article
Published: 28 August 2019
Geological Magazine (2020) 157 (3): 405–410.
..., 1980 and Pe . taitzuhoensis Lu, 1957 . Bed A also contains other fossils, including algae, brachiopods, the bivalved arthropods Tuzoia manchuriensis Resser & Endo in Resser, 1929 and Isoxys sp., worm-like animals and possible Hurdiidae (unpublished). Bed B has yielded the trilobites...
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Journal Article
Published: 01 February 1979
Journal of the Geological Society (1979) 136 (1): 71–76.
... of gastropods, bivalves, bryozoans, echinoids, calcareous algae, corals and calcareous worm tubes (Pl. 1 ~ ) . Almost a third of the biogenic material greater than 1 mm diameter is gastropod debris. None of the mol- luscan remains are of infaunal types which would require sediment in which to burrow. AU...
Journal Article
Published: 01 October 2016
Russ. Geol. Geophys. (2016) 57 (10): 1419–1436.
... with distinct Cr-spinel lamellae having drop-like Cr-spinel segregations at the ends, passing into rounded grains in diopside and neighboring olivine; d , fragment of Fig. 3 c . Hereafter, Ol, olivine, En, enstatite, Di, diopside, Amph, amphibole, and Chr, Cr-spinel. Fig. 4. X-ray spectral map 1...
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Journal Article
Published: 05 May 2020
Geological Magazine (2021) 158 (2): 199–218.
... , and the detailed field relation is described in the following. Table 1. Representative mineral analysis of olivine (Ol), orthopyroxene (Opx) and clinopyroxene (Cpx). Fe 3+ was calculated using the method outlined in Droop ( 1987 ). Subscripts: c – core; r – rim; i – interstitial; s – secondary mineral...
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Journal Article
Published: 01 February 1983
Journal of the Geological Society (1983) 140 (1): 27–37.
... an early role for the opine pathways in providing energy for the burrowing of infaunal worms of the Precambrian era. Biological rather than chemical factors are concluded to have been the main pressures for the evolution of anaerobic metabolism. D. R. L ivingstone , Institute for Marine Environmental...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1944
AAPG Bulletin (1944) 28 (7): 977–1011.
... ). Fig. 6. —Oyster growing on pebble. Bore holes of mud worm Polydora are visible at top right of oyster shell and in pebble near attachment of oyster. Each worm makes two interconnected holes in outline like a dumbbell. Natural size. Next to the clay the most common component of the beds...
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Journal Article
Published: 01 March 2006
Journal of Sedimentary Research (2006) 76 (3): 515–523.
... that coralline algae ( Stanley et al. 2002 ; Ries in press ), echinoids, serpulid worms, crabs, shrimp ( Ries 2004 ), and some species of coccolithophores ( Stanley et al. 2005 ), which naturally secrete high-Mg calcite in modern aragonite seas, actually change their mineralogy to low-Mg calcite when grown...
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