DOCSLIB.ORG

Volgian and Santonian–Campanian Radiolarian Events of the Russian Arctic and Pacific Rim

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Volgian and Santonian–Campanian Radiolarian Events of the Russian Arctic and Pacific Rim Volgian and Santonian–Campanian radiolarian events of the Russian Arctic and Pacific Rim VALENTINA S. VISHNEVSKAYA and GENRIETTA E. KOZLOVA Vishnevskaya, V.S. and Kozlova, G.E. 2012. Volgian and Santonian–Campanian radiolarian events from the Russian Arctic and Pacific Rim. Acta Palaeontologica Polonica 57 (4): 773–790. Radiolarians are widely distributed in two siliceous intervals that coincide with the Tithonian–Berriasian and Santonian– Campanian boundaries in the Mesozoic of the Russian Arctic and Pacific Rim. The first level is rich in organic matter and typical of Jurassic–Cretaceous boundary strata from the Russian North European Margin (Barents−Pechora, Volga−Urals, and Siberian hydrocarbon provinces, as well as western Kamchatka). Abundant and diverse representatives of the family Parvicingulidae provide a basis for establishing the new genus Spinicingula (uppermost Middle Volgian–Lower Berriasian); another new genus, Quasicrolanium (Upper Volgian–Upper Berriasian) is also described. A Santonian– Campanian siliceous interval with radiolarians is documented from the margins of northern Asia (eastern Polar Ural, Kara Basin, Kamchatka). The Boreal genus Prunobrachium makes its first appearance at the Santonian–Campanian boundary and reaches an acme in Campanian strata. Radiolarian data can be used for basin biostratigraphy and correlation, as well as palaeogeographical interpretation of these hydrocarbon−rich facies. The Arctic and northern Pacific rims are well cor− related on the basis of parvicingulids, while in Sakhalin these are absent and calibrations are based on Unitary Associa− tions zones of the Tethys. In addition to the two new genera noted above, five new species (Parvicingula alata, Parvicingula papulata, Spinicingula ceratina, Lithostrobus borealis, and Spongurus arcticus) are erected, while 60 radiolarian species typical of the Russian Arctic and Pacific rims are illustrated. Key words: Radiolaria, events, new taxa, organic−rich cherts, Cretaceous, northern Russia. Valentina S. Vishnevskaya [[email protected]], Geological Institute, Pyzhevsky lane 7, Moscow 119017, Russia; Genrietta E. Kozlova [[email protected]], VNIGRI, Litejnyj pr., 39, Sankt−Peterburg 191104, Russia. Received 9 July 2011, accepted 18 December 2011, available online 24 February 2012. Copyright © 2012 V.S. Vishnevskaya and G.E. Kozlova . This is an open−access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Introduction lected Eurasian basins (Blueford and Gonzales 1993) did not show any of the giant or subgiant fields of the Russian Arctic, There are four highly siliceous and organic−rich suites in exclusive of the western Siberian sedimentary basin, which Russia, which are unique and of great economic importance is predominantly located in Siberia, but not in the Arctic. The due to their high content of organic matter. The rocks of the North Sea, Norwegian Sea, and Barents Sea areas were not Domanik (Upper Devonian), Bazhenovo (Upper Jurassic represented either. and Lower Cretaceous), Kuma (Paleogene) and Maikop Radiolarian biostratigraphy is vital for hydrocarbon ex− (Neogene) suites are rich in siliceous tests of Radiolaria and ploration in these regions, because these biota often are the sponge spicules. Studies of radiolarians of Bazhenovo suite only fossils present. Because radiolarian assemblages are have allowed the compilation of provincial zonal schemes abundant and diverse, they can easily be used to constrain the and correlation with other regions. A good example and il− age of core samples from drill sites in these hydrocarbon−rich lustration of the use of radiolarians as a tool in evaluating successions. Recently, the Upper Jurassic and Lower Creta− stratigraphical and palaeoenvironmental aspects of hydro− ceous Bazhenov oil−producing sequence of western Siberia carbon−rich sedimentary basins, is a special issue of Micro− and the Kimmeridgian and Volgian bituminous beds of paleontology entitled “Radiolaria of giant and subgiant fields northern Russia have attracted special attention (Hantzper− in Asia” which was published in 1993. In that volume, the gue et al. 1998; Zakharov 2006). Similar highly bituminous emphasis was on the Asian part of the Eurasian continent; in deposits are known along the Barents Sea margin and in the consequence, the main oil and gas provinces of northern Eu− Volga−pre−Ural Basin, from Kara Sea, the Laptevs Sea mar− rope were not included. Moreover, the generalised map of se− gin and also from the Norwegian and North Seas. The origin Acta Palaeontol. Pol. 57 (4): 773–790, 2012 http://dx.doi.org/10.4202/app.2011.0040 774 ACTA PALAEONTOLOGICA POLONICA 57 (4), 2012 30° 50° 70° 90° 110° 130° 150° BEAUFORT SEA 170° 10° CHUKCHI SEA ARCTIC OCEAN 5B NORWEGIAN SEA 10° SEA 170° EAST SIBERIAN BARENTS SEA 5A LAPTEV SEA 2A KARA SEA 30° 1 2 4 3A 150° 3 40° 6 4A 60° 80° 100° 120° 140° Fig. 1. Location of some radiolarian−bearing source rocks in the Russian Arctic and along the Pacific margins; localities A and B correspond to Fig. 2. 1, Mezen Basin, Pesha section. 2, southeastern Barents−Pechora Basin: 2, Narjan−Mar, borehole 5; 2A, Kolguev, borehole 140. 3. Volga−Pre−Ural Basin: 3, Shilovka section; 3A, Gorodicshe section, Uljanovsk region. 4, Northern and western Siberian basins: 4, Polar Ural, borehole 22; 4A, Upper Salym, bore− hole 17. 5, western Kamchatka and Chukotka: 5, Palana section; 5A, Omgon; 5B, Semiglawaya Mountains. 6, Sakhalin. of the Volgian siliceous combustible shaly sequence is of Here we consider two siliceous intervals: the Volgian and great importance, so as is subject of constant discussions. the Campanian. Because siliceous bituminous rocks of the Typically, these deposits, rich in organic matter, are non−cal− Russian Arctic and along the Ural margin are part of the con− careous, hydrophobic and distinguished by higher radioac− cept of the Volgian Stage (i.e., the Bazhenovo productive ho− tivity among country rocks. Previously it has been shown rizon and others), the stratigraphic correlation of the Boreal that the Volgian combustible shaly sequences of the Bazhe− Volgian Stage with its counterpart in the Tethyan province nov suite of western Siberia and the Norwegian continental needs to be considered. Based on the views accepted by the shelf of the Barents Sea are essentially enriched relative to Interdepartmental Stratigraphic Committee of Russia (Zha− common clay rocks by organophilic elements which accom− moida and Prozorovskaya 1997), the Upper Volgian Sub− pany sapropelic organic matter: V ten times higher than nor− stage corresponds to the lower Berriasian (Lower Creta− mal, Ni six times, Cu and Zn two to three times as much as ceous), while the Middle Volgian Substage equates with the the average of Recent oceans; 60% of U, Mo, As, Sb of their Tithonian (Upper Jurassic). Thus, the Volgian siliceous in− quantity in present−day oceans (Gavshin and Zakharov terval is the highest interest with regard to the position of the 1991). It has also been noted that deposits of that kind occur Jurassic–Cretaceous boundary, which is situated between the at different stratigraphic levels in the major oil and gas bas− Middle and Upper Volgian. ins; within the Persian Gulf in the Callovian and Oxfordian, Institutional abbreviations.—GIN, Geological Institute, in the North Sea in the Kimmeridgian (Galimov 1986). For Moscow, Russia; VNIGRI, All−Russia Petroleum Research this reason, it is important to determine the chronostrati− Exploration Institute, Sankt−Peterburg, Russia. graphic position of these deposits as precisely as possible within the Volgian in the Boreal Realm, as well as to try to lo− cate its equivalents in the Tethyan Realm. Radiolarian bio− Historical background stratigraphy offers the best means to make such important chronostratigraphic correlations, because these biota are The Mesozoic radiolarians of the Russian Arctic Margin common in these oil shale sequences. In addition, radiolarian were first studied by Kozlova and Gorbovetz (1966) and biostratigraphy is well established for this time interval in the Kozlova (1971, 1983, 1994b). Three different radiolarian as− Tethyan Realm (Baumgartner et al. 1995; De Wever et al. semblages were introduced for the Jurassic (Lower Kimme− 2001) as well as in the present day California (Pessagno ridgian, Middle Volgian and Upper Volgian) of the Timan− 1977; Hull 1997; De Wever et al. 2001). Pechora region (Kozlova 1971, 1994b) and the Middle Vol− VISHNEVSKAYA AND KOZLOVA—RADIOLARIANS IN THE RUSSIAN ARCTIC 775 organic 4 marine clay basalt detritus 90 sandstone tuff sponge phosphatic siltstone concretion 3 pebble 50 location of 57 marl glauconite samples cp2 6 bituminous ammonite 5 K ap-al limestone 7-1 1 shale and belemnite cp1 Kcp2 134/01 Buchia chert pyrite Kst2 st peat, foraminifera: K br-ap jasper a, benthic; JK 1 lignite b, planktonic 3 1 cn 150 tripoli trace of radiolaria fossils Kbr 0 5B 1 5A 60 2A 3A 35 4A v-g 61 2880 v 460 syzranicus ian 0.5 Volg- v h-b 1 Kv1 4-1 2 v nodiger 0.1-0.5 G2 218 subditus 0-0.2 Kbs1 603-5 1 bs bs 603-6 Kbs1 102-1 v3 v 140 fulgens 0.5-0.8 tt -bs 125.0 5 3 2 114 v J3v 1-2 nikitini 0.3-0.5 Jtt Jtt3 2 Volgian 3 v3 3 v1 ox-km virgatus Upper Jurassic 0.8-1 km J2k zarajs- 2900 Jk2 k-tt 234 kens 6-9 G1 v2 2 1 480 2912 panderi pavlovi Volgian 2 0.5-2.5 0 pseudo- 146.0 scythica sokolovi 1 3.5-6 klimovi Volgian eudoxus 2 Kimm. 12-18 cymodoce 1 Kimm. Fig. 2. Correlation of Upper Jurassic and Cretaceous sequences from the Barents−Pechora region of the Arctic to Sakhalin in the far east of the Pacific Mar− gin. Localities: 1, Mezen Basin, Pesha section. 2, southeastern Barents−Pechora Basin: 2, Narjan−Mar, borehole 5; 2A, Kolguev, borehole 140. 3, Volga−Pre−Ural Basin: 3, Shilovka section; 3A, Gorodicshe section, Uljanovsk region.
Load more

Recommended publications
  • Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper
    Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper Chapter A of The 2008 Circum-Arctic Resource Appraisal Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey Cover. View to the east of the Lisburne well during active drilling in July 1979, Ivotuk Hills, northern Alaska. U.S. Geological Survey photo by Thomas Moore. Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper By Donald L. Gautier and Thomas E. Moore Chapter A of The 2008 Circum-Arctic Resource Appraisal Edited by T.E. Moore and D.L. Gautier Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Gautier, D.L., and Moore, T.E., 2017, Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) professional paper, chap.
    [Show full text]
  • 30. Turonian–Santonian Benthic
    Mascle, J., Lohmann, G.P., and Moullade, M. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 159 30. TURONIAN–SANTONIAN BENTHIC FORAMINIFER ASSEMBLAGES FROM SITE 959D (CÔTE D’IVOIRE-GHANA TRANSFORM MARGIN, EQUATORIAL ATLANTIC): INDICATION OF A LATE CRETACEOUS OXYGEN MINIMUM ZONE1 Ann E.L. Holbourn2,3 and Wolfgang Kuhnt2 ABSTRACT Turonian–Santonian organic-rich fissile black claystones with laminated intervals from Hole 959D on the Côte d’Ivoire- Ghana Transform Margin, drilled during Ocean Drilling Program Leg 159, contain benthic foraminifer assemblages dominated by buliminid associations. The lower Turonian assemblage from Core 159-959D-68R is strongly dominated by Bolivina anam- bra, Praebulimina sp. 1, Praebulimina sp. 2, Praebulimina sp. 3, and Gavelinella spp. The upper Turonian to lower Coniacian assemblage from Core 159-959D-67R displays low abundance and low diversity and consists mostly of organically cemented agglutinated taxa and/or some corroded tests of Lenticulina, Bolivina, Gyroidinoides ex gr. nitidus. The middle Coniacian to lower Santonian assemblage from Core 159-959D-66R and from the base of Core 159-959D-65R contains high numbers of Praebulimina robusta, Praebulimina fang, Neobulimina subregularis, and Buliminella cf. gabonica, but shows marked fluctua- tions in abundance and diversity, which appear to be related to changes in total organic carbon. The distinct composition of the two buliminid associations in Core 159-959D-68R and Core 159-959D-66R suggests that endemism was stronger during the early Turonian, when circulation was probably more restricted and connections between equatorial Atlantic basins were lim- ited. We interpret the late Coniacian–early Santonian depositional environment to be an oxygen minimum zone in a more open marine outer shelf or upper slope setting.
    [Show full text]
  • Cenomanian Turonian Coniacian Santonian Campanian
    walteri aff. aff. spp. spp. imperfectus spp. (prisms) Chronostratigraphy Offshore Norway sp. 1 Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Allomorphina halli / pyriformis Sigmoilina antiqua Textularia Gavelinella intermeda gracillima Valvulineria Bulbobaculites problematicus Caudammina ovuloides Nuttallinella florealis Stensioeina granulata polonica Inoceramus Rzehakina minima Rzehakina epigona Fenestrella bellii Gaudryina filiformis Trochamminoides Haplophragmoides Gavelinella usakensis Caudammina ovula Coarse agglutinated spp. LCO dubia Tritaxia Plectorecurvoides alternans Reussella szajnochae Recurvoides Hippocrepina depressa Psammosphaera sphaerical radiolarians Ma Age/Stage Lingulogavelinella jarzevae elegans Lt NCF19 Maastrichtian volutus LCO 70 NCF18 E szajnochae dubia Lt 75 LCO of NCF17 Campanian Deep Water M Agglutinated 80 Foraminifera E bellii NCF16 Lt Inoceramus LCO NCF15 85 Santonian M E polonica NCF14 Lt Coniacian M E Marginotruncana NCF13 90 Lt Turonian M E Dicarinella NCF12 95 Lt brittonensis M NCF11 Cenomanian delrioensis LCO NCF10 E antiqua NCF9 100 Figure 2.8c. Stratigraphic ranges of Upper Cretaceous benthic foraminifera, and miscellaneous index taxa, oshore mid-Norway, with the foraminiferal zonation established in this study. s.l. Chronostratigraphy Offshore Norway Geologic Time Scale 2012 Zonation (Gradstein et al., 1999, and this study) Abathomphalus mayaroensis Pseudotextularia elegans Hedbergella planispira Hedbergella hoelzi Praeglobotruncana delrioensis Praeglobotruncana stephani
    [Show full text]
  • The Valanginian to Aptian Stages - Current Definitions and Outstanding Problems
    © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 4‘>3 Zitteliana 10 493-500 München, I. Juli 1983 ISSN 0373 9627 The Valanginian to Aptian stages - current definitions and outstanding problems Compiled by PETER FRANKLIN RAWSON») Willi 3 tables ABSTRACT Current definitions of the Valanginian to Aptian Stages are tion potential. The I’re-Albian Stages Working Croup is in­ reviewed and some of the outstanding problems outlined. Fi­ stigating study of selected sections in various parts of the nal recommendations on stage boundaries can be made only world to provide an integrated framework ol biostraligraphy after much more strat¡(graphical work has been completed, as and event stratigraphy. the eventual boundaries must have good international correla­ KURZFASSUNG Lin Überblick über die gängigen Definitionen der Stufen barsein. Die Prc-Albian Stagcs Working Group regt an, ms vom Valangin bis zum Apt wird gegeben und einige wichtige gewählte Profile in verschiedenen Peilen der Welt zu unterst! Probleme hervorgehoben. Lndgülligc Empfehlungen zu Stu­ ehen, um so den allgemeinen Rahmen liii eine Ncudelinition fengrenzen sind z. Zt. noch nicht möglich. Dazu sind noch der Stufen auf der Grundlage der Biostraligraphie und der weitere stratigraphische Untersuchungen erforderlich, denn Lvenl-Straiigraphic zu schaffen. die fcstzulcgendcn Grenzen müssen international korrelier­ I. INTRODUCTION This review has been compiled on behalf of the Prc-Albian boundaries and to improve the usage of stage names in re­ Stages Working Group of the Subcommission on Cretaceous gions away from stratotype sections." Stratigraphy. The primary role of the working group is to cla ­ Thus our fundamental philosophy is first to make objective rify, and to improve where necessary, the definition and correlations between regions and only then to redefine stages boundaries of the Valanginian to Aptian Stages.
    [Show full text]
  • Stratigraphy of Deep-Water Cretaceous Deposits in Gyangze, Southern Tibet, China ) Xianghui Lia, , Chengshan Wangb, Xiumian Huc
    Cretaceous Research 26 (2005) 33–41 www.elsevier.com/locate/CretRes Stratigraphy of deep-water Cretaceous deposits in Gyangze, southern Tibet, China ) Xianghui Lia, , Chengshan Wangb, Xiumian Huc aState Key Laboratory of Oil-Gas Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, PR China bChina University of Geosciences, 29 Xueyuan Lu, Beijing 100083, PR China cDepartment of Earth Sciences, Nanjing University, Nanjing 210093, PR China Accepted in revised form 15 November 2004 Available online 12 January 2005 Abstract Extensive tectonic activity in southern Tibet (Tibetan Tethys Himalayas) resulted in overthrusting and tectonic deformation of Cretaceous strata, which in the study area was not recognized by earlier researchers. Field studies of three typical cross-sections in southern Tibet has led to the revision of previous stratigraphy. The thickness of the Cretaceous in Gyangze varies between 300 and 700 m, but is not over 2000 m as previously estimated at Gyabure and Weimei, where the strata are overturned and repeated owing to previously unrecognized thrusts. In upward stratigraphic order four lithological markers were used in the field study: belemnite and black marker, lenticular limestone and white marker, red marker, and olistolith marker. The first two of these are associated with the fine-grained clastic shelf sequence of the Gyabula Formation, which is of Berriasian–early Santonian age. The third is the deep-sea red-beds marker of the Chuangde Formation, dated as middle Santonian–early Campanian. The fourth depicts the slump facies and olistolith of the middle Campanian–Paleocene Zongzhuo Formation. The revised Cretaceous stratigraphy provides a framework for studies of the pelagic red beds of the Chuangde Formation, which is intermittently exposed in southern Tibet.
    [Show full text]
  • Upper Cenomanian •fi Lower Turonian (Cretaceous) Calcareous
    Studia Universitatis Babeş-Bolyai, Geologia, 2010, 55 (1), 29 – 36 Upper Cenomanian – Lower Turonian (Cretaceous) calcareous algae from the Eastern Desert of Egypt: taxonomy and significance Ioan I. BUCUR1, Emad NAGM2 & Markus WILMSEN3 1Department of Geology, “Babeş-Bolyai” University, Kogălniceanu 1, 400084 Cluj Napoca, Romania 2Geology Department, Faculty of Science, Al-Azhar University, Egypt 3Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Sektion Paläozoologie, Königsbrücker Landstr. 159, D-01109 Dresden, Germany Received March 2010; accepted April 2010 Available online 27 April 2010 DOI: 10.5038/1937-8602.55.1.4 Abstract. An assemblage of calcareous algae (dasycladaleans and halimedaceans) is described from the Upper Cenomanian to Lower Turonian of the Galala and Maghra el Hadida formations (Wadi Araba, northern Eastern Desert, Egypt). The following taxa have been identified: Dissocladella sp., Neomeris mokragorensis RADOIČIĆ & SCHLAGINTWEIT, 2007, Salpingoporella milovanovici RADOIČIĆ, 1978, Trinocladus divnae RADOIČIĆ, 2006, Trinocladus cf. radoicicae ELLIOTT, 1968, and Halimeda cf. elliotti CONARD & RIOULT, 1977. Most of the species are recorded for the first time from Egypt. Three of the identified algae (T. divnae, S. milovanovici and H. elliotti) also occur in Cenomanian limestones of the Mirdita zone, Serbia, suggesting a trans-Tethyan distribution of these taxa during the early Late Cretaceous. The abundance and preservation of the algae suggest an autochthonous occurrence which can be used to characterize the depositional environment. The recorded calcareous algae as well as the sedimentologic and palaeontologic context of the Galala Formation support an open-lagoonal (non-restricted), warm-water setting. The Maghra el Hadida Formation was mainly deposited in a somewhat deeper, open shelf setting.
    [Show full text]
  • Late Cretaceous (Santonian-Campanian) Stratigraphy of the Northern Sacramento Valley, California
    Late Cretaceous (Santonian-Campanian) stratigraphy of the northern Sacramento Valley, California DcT^rf {Department of Geology, University of California at Davis, Davis, California 95616 rElbK L). WAKL) J ABSTRACT INTRODUCTION METHODS The Upper Cretaceous (Coniacian-lower Thick accumulations of Upper Cretaceous Strata of the Chico Formation dip gently to Campanian) Chico Formation of the north- sedimentary deposits are found on the western, the southwest. Sections were mejisured using eastern Sacramento Valley, California, includes northern, and eastern margins of the Great Val- either tape and compass or Jacob's staff. In some three newly defined members at the type local- ley of California (Fig. 1). The search for oil and areas, outcrop data were plotted on U.S. Geo- ity: (1) cobble conglomerate of the basal Pon- gas in northern California, as well as interest in logical Survey topographic quadrangles and derosa Way Member, (2) coarse-grained con- the processes of sedimentation in fore-arc re- stratigraphie columns were determined trigo- glomeratic sandstone of the overlying Musty gimes, has made the Great Valley seque nce, ex- nometrically. Paleontologic collections of mac- Buck Member, and (3) fine-grained silty sand- posed along the west side of the Sacramento rofossils were made during the measuring of stone of the uppermost Ten Mile Member. Valley, probably the best-studied fore-arc de- sections. Minor offset of bedding was observed Other outcrops of the Chico Formation exhibit posit in the world (Ojakangas, 1968; Dickinson, on more southerly exposures of the Chico For- the same three members plus an additional unit, 1971; Ingersoll, 1978, 1979). These workers in- mation, and such structural modification be- the Kingsley Cave Member, composed of mud- terpreted strata of the Great Valley sequence to comes more prominent farther north.
    [Show full text]
  • Fe1ca349ca6c1561de7ea7ba19
    Research Paper GEOSPHERE Latest Neoproterozoic to Cambrian detrital zircon facies of western Laurentia GEOSPHERE; v. 14, no. 1 William Matthews, Bernard Guest, and Lauren Madronich Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, Alberta T2N 1N4, Canada doi:10.1130/GES01544.1 11 figures; 1 table; 1 supplemental file ABSTRACT 1963; Bond and Kominz, 1984; Lickorish and Simony, 1995; Fedo and Cooper, 2001), and are exposed along the length of the Cordillera from Mexico to the CORRESPONDENCE: [email protected] Late Neoproterozoic to Cambrian sandstone units are common in west- Northwest Territories of northern Canada (Stewart et al., 2001; Hadlari et al., ern Laurentia and record initial transgression of the craton after the for- 2012). These strata record the initial transgression of the Laurentian craton CITATION: Matthews, W., Guest, B., and Madronich, mation of the western passive margin during the latest Neoproterozoic to following the onset of thermal subsidence (Bond and Kominz, 1984; Bond et L., 2018, Latest Neoproterozoic to Cambrian detrital zircon facies of western Laurentia: Geosphere, v. 14, earliest Cambrian. Detrital zircon measurements from 42 latest Neopro- al., 1984, 1985; Levy and Christie-Blick, 1991; Yonkee et al., 2014) and cover an no. 1, p. 243–264, doi:10.1130/GES01544.1. terozoic to Cambrian basal Sauk sequences and five older Neoproterozoic important period in the evolution of complex life (Marshall, 2006). sandstone samples from a region extending from the Mexico–United States The widespread occurrence of sandstone facies suitable for detrital zircon Science Editor: Shanaka de Silva border to central British Columbia, Canada, are combined with previous re- geochronology, and the relatively limited time span of their deposition, make Associate Editor: Christopher J.
    [Show full text]
  • Norwegian Seaway: a Key Area for Understanding Late Jurassic to Early Cretaceous Paleoenvironments
    CORE Metadata, citation and similar papers at core.ac.uk Provided by OceanRep PALEOCEANOGRAPHY, VOL. 18, NO. 1, 1010, doi:10.1029/2001PA000625, 2003 The Greenland-Norwegian Seaway: A key area for understanding Late Jurassic to Early Cretaceous paleoenvironments Jo¨rg Mutterlose,1 Hans Brumsack,2 Sascha Flo¨gel,3 William Hay,3 Christian Klein,1 Uwe Langrock,4 Marcus Lipinski,2 Werner Ricken,5 Emanuel So¨ding,3 Ru¨diger Stein,4 and Oliver Swientek5 Received 22 January 2001; revised 24 April 2002; accepted 9 July 2002; published 26 February 2003. [1] The paleoclimatology and paleoceanology of the Late Jurassic and Early Cretaceous are of special interest because this was a time when large amounts of marine organic matter were deposited in sediments that have subsequently become petroleum source rocks. However, because of the lack of outcrops, most studies have concentrated on low latitudes, in particular the Tethys and the ‘‘Boreal Realm,’’ where information has been based largely on material from northwest Germany, the North Sea, and England. These areas were all south of 40°N latitude during the Late Jurassic and Early Cretaceous. We have studied sediment samples of Kimmeridgian (154 Ma) to Barremian (121 Ma) age from cores taken at sites offshore mid-Norway and in the Barents Sea that lay in a narrow seaway connecting the Tethys with the northern polar ocean. During the Late Jurassic-Early Cretaceous these sites had paleolatitudes of 42–67°N. The Late Jurassic-Early Cretaceous sequences at these sites reflect the global sea-level rise during the Volgian-Hauterivian and a climatic shift from warm humid conditions in Volgian times to arid cold climates in the early Hauterivian.
    [Show full text]
  • Cretaceous Research 69 (2017) 49E55
    Cretaceous Research 69 (2017) 49e55 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes High-resolution calcareous nannofossil biostratigraphy of the Santonian/Campanian Stage boundary, Western Interior Basin, USA * Zachary A. Kita a, , David K. Watkins a, Bradley B. Sageman b a Department of Earth and Atmospheric Sciences, University of Nebraska, Lincoln, NE 68588, USA b Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL 60208, USA article info abstract Article history: The base of the Campanian Stage does not have a ratified Global Stratotype Section and Point (GSSP); Received 26 June 2016 however, several potential boundary markers have been proposed including the base of the Scaphites leei Received in revised form III ammonite Zone and the base of the paleomagnetic Chron C33r. Calcareous nannofossil assemblages 25 August 2016 from the Smoky Hill Member of the Niobrara Formation in the central Western Interior Seaway, USA Accepted in revised form 28 August 2016 were analyzed from two localities to determine relevant biohorizons and their relationships to these Available online 30 August 2016 potential boundary markers. In a previous study, the Aristocrat Angus 12-8 core (Colorado) was astro- chronologically dated and constrained using macrofossil zonations and radiometric ages. The Smoky Hill Keywords: Calcareous nannofossils Member type area (Kansas) provides an expanded interval with good to excellent nannofossil Biostratigraphy preservation.
    [Show full text]
  • Berriasian Planktonic Foraminifera and Calcareous Nannofossils from Crimea Mountains, with Reference to Microfossil Evolution
    Swiss Journal of Palaeontology (2019) 138:213–236 https://doi.org/10.1007/s13358-018-0175-8 (0123456789().,-volV)(0123456789().,-volV) REGULAR RESEARCH ARTICLE Berriasian planktonic foraminifera and calcareous nannofossils from Crimea Mountains, with reference to microfossil evolution 1 2 3 4 1 5 F. M. Gradstein • A. Waskowska • L. Kopaevich • D. K. Watkins • H. Friis • J. Pe´rez Panera Received: 26 July 2018 / Accepted: 22 October 2018 / Published online: 7 November 2018 Ó The Author(s) 2018 Abstract A Berriasian age planktonic foraminifera assemblage from a section near the village of Krasnoselivka in the Tonas River Basin, Crimea contains Favusella hoterivica (Subbotina), ?Favusella sp., Conoglobigerina gulekhensis (Gorbachik and Poroshina), Lilliputinella eocretacea (Neagu), Lilliputinella aff. similis (Longoria), Hedbergella aff. handousi Salaj and ? Globuligerina sp. Specimens are poorly preserved, but test morphology, aperture and key wall texture features are recognizable. Age assignment is based on a diverse and well-preserved calcareous nannofossils assemblage of upper zone CC2 and ammonites (Jacobi Zone). The nannfossils indicate an open marine environment of Tethyan affinity. Several of the planktonic foraminiferal taxa were not previously described from pre-Valanginian or Hauterivian strata. XRD analysis of the tests of benthic and planktonic foraminifera and micro-gastropods shows these to be calcitic in composition, also of those benthic and planktonic foraminifera that were deemed to be originally aragonitic in composition, indicating dia- genetic changes in carbonate fractions. From detailed comparison to Jurassic planktonic foraminifera, two lineages are proposed from Late Jurassic into earliest Cretaceous: Globuligerina oxfordiana (Grigelis) to Favusella hoterivica (Sub- botina) and Globuligerina balakhmatovae (Morozova) to Lilliputinella eocretacea (Neagu).
    [Show full text]
  • Uppermost Campanian–Maestrichtian Strontium Isotopic, Biostratigraphic, and Sequence Stratigraphic Framework of the New Jersey Coastal Plain
    Uppermost Campanian–Maestrichtian strontium isotopic, biostratigraphic, and sequence stratigraphic framework of the New Jersey Coastal Plain Peter J. Sugarman New Jersey Geological Survey, CN 427, Trenton, New Jersey 08625, and Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903 Kenneth G. Miller Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903, and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964 David Bukry U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025 Mark D. Feigenson Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903 ABSTRACT boundaries elsewhere in the Atlantic Recent stratigraphic studies have concen- Coastal Plain (Owens and Gohn, 1985) and trated on the relationships between these se- Firm stratigraphic correlations are the inferred global sea-level record of Haq quences, their bounding surfaces (unconfor- needed to evaluate the global significance of et al. (1987); they support eustatic changes mities), and related sea-level changes. The unconformity bounded units (sequences). as the mechanism controlling depositional shoaling-upward sequences described by We correlate the well-developed uppermost history of this sequence. However, the latest Owens and Sohl (1969) have been related to Campanian and Maestrichtian sequences Maestrichtian record in New Jersey does recent sequence stratigraphic terminology of the New Jersey Coastal Plain to the geo- not agree with Haq et al. (1987); we at- (e.g., Van Wagoner et al., 1988) by Olsson magnetic polarity time scale (GPTS) by in- tribute this to correlation and time-scale (1991) and Sugarman et al. (1993). Glauco- tegrating Sr-isotopic stratigraphy and bio- differences near the Cretaceous/Paleogene nite beds are equivalent to the condensed stratigraphy.
    [Show full text]