 | | Journal (article/letter/editorial) | | of Bohemia differ from those of North-western Germany in not comprising a calcareous Downloaded from...therefore, been referred by native geologists to the Roth-todt-liegende, or what I call Lower Permian. Being...composed, he shows how the lowest member of the ' Roth-liegende,' or h i s ' conglomerate,' dips away from...most recent, however, of the descriptions of the Roth-liegende of this tract is by M. Jokely, and was...furnished by M. Haidinger, as stated above) divides the Roth-liegende into three principal parts. The uppermost |  | | Journal (article/letter/editorial) | | Schrollianus. These are conformably overlain by white Roth-Dolomite, with Myophoria fallax. Porphyritic tufa...with porphyritic tufa, which, again, is overlain by Roth-Dolomite, with M. fallax. The limestone contained...thickness about 150 feet. ' b. Upper Bunter-Sandstein or Roth, red shales, with white Dolomite and marls, containing...fall of small cavities, and rests conformably on Roth. It contains no fossils. t. The Chorzow Beds have...Upper Silesian Muschelkalk with that of Western Germany, we find the greatest affinity to exist as regards |  | | Report (issue) | | and Lozo (1951, p. 120) from exposures near Waco marl. Where fresh, the chalk is pale blue gray to in...tion in southern McLennan County, Tex. However, and marl which rest with slight disconformity on the as a...strata of central Texas, Adkins and I by the Taylor Marl (=Sprinkle Formation of Young, Lozo (1951, p. 119-120)...(5) of the Oak Haven Waterfall locality). Burditt Marl, and (6) "Big House Chalk;" (see Farther westward...see also Pessagno, 1969, p. 72-73), and Burditt Marl, as defined by Adkins (1933, p. 449-450) and herein |  | | Journal (article/letter/editorial) | | England . and of deposits of a similar age in Germany and America. The genus Cypridea was proposed by...Roemer and Dunker from the Wealden of England and Germany, and by them assigned to Cypris. Bosquet noted...Roemer (1839) described and figured species from Germany he identified with C. valdensis, C. tuberculata...Pseudocypridina Roth, 1933. Distinguished by the absence of a "notch." Genotype: P. piedmonti Roth, 1933. See...from Germany (see Koert, 1898; Wieher, 1940, and Martin, 1940) and America (see Jones, 1893; Roth, 1933; |  | | Journal (article/letter/editorial) | | and Semil on the N.N.W. These roeks, simply termed Roth-todt-liegende by the Austrian and Saxon geologists...inferior half only of these deposits, or the lower Roth-liegende, has actually been sunk through by a shaft...in proceeding from north to south (in Eastern Germany), the Zeehstein thins out; and seeing the vast...that some of the higher members of the Bohemian Roth-liegende may represent that limestone in time. The...time becoming thicker, while at Aveling the Oolite Marl is first seen interposed between the Lower Ragstone |  | | Journal (article/letter/editorial) | | memoir on the Hartz, that the Permian groups of Germany and this country can be strictly contemporanized...whether these subdivisions are represented in Germany. As far, however, as the present examination extends...its history,--on the other hand, in this part of Germany, if we are to judge by uniformity of mineral character...threefold division of the Bunter in other parts of Germany. ~- Elementary Geology., 5th edit. p. 573. [Nov...2016 1857.] HULL~TRIAS AND P E R M I A N . 221 Roth-todt-liegendes, and in the latter, according to |  | | Journal (article/letter/editorial) | | ~ III::.:'.':.:I :~" - ~ ~ 7 S @ L i m y marl a n d shale {'1"alia bed) with N. p.tukhian!. ...(Discoastersaipanensis Zone). 11, 12. Cvclicargolithusftoridanus (Roth and Hay), Maadi Formation, sample 37 (Chiasmolithus...oamaruensis Zone). 13. Cyclicargolithusftoridanus (Roth and Hay), Maadi Formation, sample 41 (lsthmolithus...Martini (1971) recognized this zone (NP 14) from Germany to represent the interval from the first occurrence...authors (Bukry and Bramlette, 1970; Bukry, 1971, 1973; Roth et al., 1971; Kerdany et al., 1974; Proto Decima |  | | Journal (article/letter/editorial) | | lower Zechstein near Korbach (northwestern Hesse, Germany). It includes therapsids (cynodonts and dicynodonts)...SCUAtSMI3ERC 1985) and its English equivalent, the Marl Slate, as well as the sandstones of the Cutties...verified (HAuBOLD ~ SCHAUMI3ERG 1985). The correlative Marl Slate of Durham has yielded Coelurosauravusjaekeli...dated as early Tatarian (MENNING 1986, 1991). In Germany, the Illawarra Reversal occurs in the upper Rotliegend...in both the basal Zechstein of England (Marl Slate) and Germany (Kupferschiefer) and the Lower Sakamena |  | | Journal (issue) | | to the world famous Radoboj machine construction. Marl, which was the body carrying sulfur material (Figure...to Sarmatian). The variety of fauna captured in marl is rich, ranging from shells to fishes and whales...Geological samples from Radoboj: (left) sulphur in marl – finding of König Friedrich August II von Sachsen...essential aspects of geology to the general public in Germany. Each year, a specific type of rock is chosen to...geosciences, about geology and petrography in Germany, and about the rock industry. In 2019, the choice |  | | Journal (article/letter/editorial) | | PALEOGEOLOGY OF THE PANHANDLE OF TEXAS By ROBERT ROTH CONTENTS Page Abstract 1671 Deny Strawn Acknowledgment...more easily recognized un1671 1672 ^ < ROBERT ROTH—PALEOGEOLOGY OF THE PANHANDLE OF TEXAS STANDARD...cross-section C-C' (PI. 3). The line of sec- 1674 ROBERT ROTH—PALEOGEOLOGY OF THE PANHANDLE OF TEXAS FIGURE 3...comparative lithologic characteristics. 1676 ROBERT ROTH—PALEOGEOLOGY OF THE PANHANDLE OF TEXAS FIGURE 5...crystalline limestone, white to light-gray dolomite, minor marl with green cast, and translucent chert. Minute grains |  | | Journal (article/letter/editorial) | | grayish-white limestone containing numerous chert and marl horizons. Although overlapping portions of the sections...interval below 100 m contains numerous green silicified marl layers which are mostly less than 5 cm thick. Many...have black, cherty cores, interbedded shale and marl are usually quite rare in the Maiolica at Caprioio...10 m). It consists of green, red and gray shaly marl with a few thin limestone beds. Individual hmestone...separated by an interval of alternating limestone and marl [2,18]. The top of the uppermost bed of Maiolica |  | | Journal (article/letter/editorial) | | probably sedimented in the form of copepod pellets (Roth et al. 1975). The uniformity of primary production...variations in the clay: carbonate content producing chalk-marl rhythms; omission surfaces due to minor breaks in...to slight early diagenetic hardening; thin clay/ marl beds derived from detrital or volcanically sourced...below). Time-series analysis of Cenomanian chalk-marl bedding couplets indicates that the precessional...Because bedded flints display similar spacing to chalk-marl couplets, and also may show 'bundling' suggestive |  | | Journal (article/letter/editorial) | | ositional solutio n ha s produced wispy-flasers of marl in the cha lk, and ha s preferentiall y rem oved...more there are em thick beds of very argillaceous marl. In addition, the lowest 25-60 m of the Chalk, provided...is pre-Coniacian, is usually developed as chalk-marl facies. This shows rhythmic alternations between...montmorillonite in the Maastrichtian of north Germany by Valeton (1960), and as Hallam & Sellwood (1968)...is a widespread a uthigenic accesso ry in chalk-marl facies, and can be found sporadicall y in white-chalk |  | | Journal (article/letter/editorial) | | consists of alternating green to cream coloured marl and micritic limestone that becomes detrital (calciturbidites)...tools has been well summarized in recent studies by Roth (1983), Cooper (1989, Bralower et af. (1989) and...Lithological symbols: 1 = shale or marl; 2 = micritic limestone; 3 = alternation of marl and micritic limestone;...534A) by Worsley (1971), Wilcoxon (1972), Roth (1983) and Roth et al. (1983). However, Thierstein (1971;...bollii to define the top of this zone. However, Roth (1978) informally defined his NC3 Zone by the first |  | | Journal (article/letter/editorial) | | reduction of petrolenni into gas. Fritz Diirr, Munich, Germany. 446.004.-Method of producing colored impressions...Schorr, Wiirteniberg, Germany. 44G.O09.-Yellow dye. William Pfitzinger, Elberfeld, Germany. A dye prepared... I ~li(lui~lizi~ig II~~ ~ i i i l k , G w r g e Roth, Higlilanrl, Ill. f o r nidcing the sanie. ,Joseph...etc. Carl A. E. Miinicke, Claustliai. Prussia, Germany. 44B,ljB.-Filter. J o h n 9. Roake, Hroc~lilyn:S...Elbridge. Composed of jute, Portland cement and marl. Issued February f7th, f N f . 446,458.-Cement |  | | Journal (article/letter/editorial) | | Aksmanice are devoid of the sub-Menilite Globigerina Marl Member, which is widespread in the Carpathian area...orogenic belt created during the Alpine orogeny; Roth and Hanzlikova, 1982). The deposition of dark shales...colour indicates Globigerina Marl Member and their equivalent – Leluchów Marl Member, grey colour denotes...non-calcareous, greenish, pale and dark) with blocks of marl. Some of the mudstones contain gastropod and mollusc...(Kotów Chert Member), grey siliceous marls (Dynów Marl Member) and black siliceous shales with thin-bedded |  | | Journal (article/letter/editorial) | | crystal elongationparallel to underlying Carnallitic Marl. the contact, suggestingflow to compensatefor the...drilling. GEOLOGY OF BOULBY POTASH MINE the Rotten Marl), reddish brown in color, is com- Table 1. Stratigraphy...presentin boreholesto the south. The Carnallitic Marl is a very weak rock, there being no physical bondingbetweenthe...Anhydrite Upgang Formation Staintondale group Marl Upper Permian (Boulby Potash) Boulby Halite BellinghamMain...group carbonate in this rock, which makes the term "marl" is further weakened by numeroussteeply dipping |  | Casson, Max, Cavin, Lionel, Jeremiah, Jason, Bulot, Luc G., Redfern, Jonathan (2018) Fishing in the Central Atlantic, an earliest Cenomanian ichthyodectiform from DSDP Site 367, Cape Verde Basin. Journal of Vertebrate Paleontology, 38 (5) doi:10.1080/02724634.2018.1510415 | Journal (article/letter/editorial) | | 41 Site 367 at the IODP Bremen Core Repository, Germany (Fig. 1A). The core was recovered from a well drilled...preserved on the bedding surface of a bituminous marl. Reports from the DSDP expedition had previously...events and nannofossil (NF) subzone after Roth (1978) and Roth et al. (1983). Subfacies A and B described... Kuhlmann at the IODP Bremen Core Repository, Germany, for his access to the data and hospitality at...the American Museum of Natural History 158:83–172. Roth, P. H. 1978. Cretaceous nannoplankton biostratigraphy |  | | Report (issue) | | and Booth, Tubulibairdia Swartz, Phanassymetria Roth, Pachydomella Ulrich, Spinobairdia Morris and Hill...lower Paleozoic specimens. Drs. Karl Krommelbein, Germany, and Vladimir Pokorny, Czechoslovakia, donated...Lalicker, 1935; Moore, 1929; Payne, 1937; Roth, 1928; Roth, 1929a ; Scott and Borger, 1941 ; Tasch, 1953...McLaughlin, 1952; Marple, 1952; Moore, 1929 ; Roth, 1929a ; Roth and Skinner, 1930 ; Scott, 1944a ; Scott...Harlton, 1929a ; Harlton, 1933 ; Roth, 1928 ; Roth, 1929a; Roth, 1929b ; Roth and Skinner, 1930; Scott, 1944a |  | | Report (issue) | | Paleontology, v. 2, no. 3, p. 246-252, 258^-259. Roth, 1929 [part], Wagner Free Inst. Sci Pub. 1, p. 31-36...553639 O -6Z -Z FIGURE 18. Amphissites costatus Roth, 1929, a restoration by Miss Carolyn Bartlett, approximately...pi. 3, fig. 4. Tournaisian-Visean, Belgium and Germany. Sohn, 1954, U.S. Geol. Survey, Prof. Paper 264-A...Mountains, Tex. AmpMssites centronota var. transversa Roth, 1929, Wagner Free Inst. Sci. Pub. 1, p. 52, pi..., Fayette County, 111. TAmpMssites marginiferus Roth. Harlton, 1933, Jour. Paleontology, v. 7, p. 23 |  | | Journal (article/letter/editorial) | | the Cretaceous of the island of Rtigen (north Germany). These he believed to be o f inorganic origin... g. THIERSTEIN 1971, 1973, 1976; SISSINGH 1977; ROTH 1978). These were summarized in most useful compilations...palaeoceanographic and palaeoclimatic questions (e.g. ROTH & BOWDLER 1981; ROTH & KRUMBACH 1986; MUTTERLOSE 1987; WATKINS...Subsequently these zonations were refined (e. g, HAQ 1983; ROTH et al. 1983; CRUX 1984; BOWN 1987; BRALOWER et al...Sea was refined and extended to the NW Atlantic by ROTH (1978). PERCH-NIELSEN (1979, 1985) summarized the |  | | Journal (article/letter/editorial) | | Poland: pyrite-marcasite nodules * E.C. Jowett 1, T. Roth 1, A. Rydzewski 2 and S. Oszczepalski 2 1 Department...Although background values exist for East and West Germany (R6sler et al. 1968; Marowsky 1969), diagnostic...lacking. This paper is an outgrowth of the work of Roth (1989) and represents part of an ongoing study to...Kupferschiefer is a carbonaceous black shale or marl at the base of the Late Permian marine-evaporite...u r c e Rote Fiiule and metal zoning In East Germany and southwestern Poland, economic Kupferschiefer |  | Eldrett, James S., Ma, Chao, Bergman, Steven C., Ozkan, Aysen, Minisini, Daniel, Lutz, Brendan, Jackett, Sarah-Jane, Macaulay, Calum, Kelly, Amy E. (2015) Origin of limestone–marlstone cycles: Astronomic forcing of organic-rich sedimentary rocks from the Cenomanian to early Coniacian of the Cretaceous Western Interior Seaway, USA. Earth and Planetary Science Letters, 423. 98-113 doi:10.1016/j.epsl.2015.04.026 | Journal (article/letter/editorial) | | limestones (ave. bed thickness ∼49 cm) with thin marl beds (ave. thickness ∼9 cm) and rare bentonites...Ford Group (Gr) is characterized by organicrich marl beds (ave. thickness ∼72 cm), thinner limestone...differences are observed both between and within marl and limestone lithofacies in all three units (Buda...relatively less depleted values compared to the marl samples with a very weak positive correlation 102...Planetary Science Letters 423 (2015) 98–113 Fig. 3. Marl and limestone facies from the Iona-1 core. a. White |  | | Report (volume) | | Formation ~RIPLEY ~MATION RIPLEY FORMATION BLUFFPORT MARL - -MEMBER --- DEMOPOLIS FORMATION DEMOPOLIS FORMATION...a dark- to blue-gray, slightly micaceous, chalky marl. An increase in sand content near the base of the...approximately 0.6 meter thick, separated by 0.75 meter of marl. To the east in Dallas County, Ala., the Arcola...consists of a number of limestone beds separated by marl units. Immediately above the Arcola, the basal Demopolis...but they are abundant and well preserved in the marl between the indurated beds. Demopolis Formation |  | | Journal (article/letter/editorial) | | Lower Oligocene~0 at Silberberg, near Helmstedt (Germany) PIETER MARKS and ERIE JAN VAN VrSSEM, Utrecht*...marine Lower, Middle and Upper Headon Beds. In Germany, the ~,typical<< Latdorf beds represent the result...base or the top of the ,,Latdorf Formation,, in Germany; the base of the Grimmertingen Sands or the base...MOORKENS 1969) an the Red Bluff Clay in Alabama (RoTH 1968) all of which are characterized by the E. subdisticha...the zonations of HAY et al. (1966, 1967) and of ROTH (1969) and is followed in turn by the Cyclococcolithus |
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