Stratigraphic and Geochemical Expression of Barremian – Aptian
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- . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? .... -
Stratigraphic and Geochemical Expression of Barremian–Aptian Global Climate Change in Arctic Svalbard
Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard Vickers, Madeleine; Price, Gregory D.; Jerrett, Rhodri; Watkinson, Matthew Published in: Geosphere DOI: 10.1130/GES01344.1 Publication date: 2016 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Vickers, M., Price, G. D., Jerrett, R., & Watkinson, M. (2016). Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard. Geosphere, 12(5), 1594-1605. https://doi.org/10.1130/GES01344.1 Download date: 26. sep.. 2021 Research Paper GEOSPHERE Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard GEOSPHERE; v. 12, no. 5 Madeleine L. Vickers1, Gregory D. Price1, Rhodri M. Jerrett2, and Matthew Watkinson1 1School of Geography, Earth and Environmental Sciences, Plymouth University, Drake Circus, Plymouth, Devon PL4 8AA, UK doi:10.1130/GES01344.1 2School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Williamson Building, Oxford Road, Manchester M13 9PL, UK 5 figures; 2 supplemental files ABSTRACT island have been difficult, and precise, high-resolution dating of this succes- CORRESPONDENCE: madeleine .vickers@ plymouth sion has not been possible. This has meant that fully interpreting the conflict- .aca.uk Significant changes in global climate and carbon cycling occurred during the ing paleo climatic evidence from this Early Cretaceous succession has not been Early Cretaceous. This study examines the expression of such climatic events in possible in a global context; therefore, this paleo–high-latitude site has been of CITATION: Vickers, M.L., Price, G.D., Jerrett, R.M., and Watkinson, M., 2016, Stratigraphic and geo- high-latitude Svalbard together with the stratigraphic utility of carbon-isotope limited use for understanding Early Cretaceous global climate change. -
Petrography and Sedimentology of the Slottsmøya Member at Janusfjellet, Central Spitsbergen 89
NORWEGIAN JOURNAL OF GEOLOGY Petrography and sedimentology of the Slottsmøya Member at Janusfjellet, central Spitsbergen 89 Petrography and sedimentology of the Slottsmøya Member at Janusfjellet, central Spitsbergen Marine Collignon & Øyvind Hammer Collignon, M. & Hammer, Ø.: Petrography and sedimentology of the Slottsmøya Member at Janusfjellet, central Spitsbergen. Norwegian Journal of Geology, Vol. 92, pp. 89-101. Oslo 2002. ISSN 029-196X. The Slottsmøya Member (Agardhfjellet Formation) in Svalbard is composed mainly of marine grey shales deposited on a slightly dysoxic and shallow shelf (offshore transition), in Volgian (Late Jurassic) to Ryazanian and possibly earliest Valanginian (Early Cretaceous) time. We present detailed lithostratigraphic, mineralogical, chemical and magnetic susceptibility logs of the Slottsmøya Member at Janusfjellet, Central Spitsbergen , providing a high-resolution stratigraphic framework for the ongoing palaeontological and geological investigations in this area. A condensed section has been recognised in the upper part of the member, based on chemical, mineralogical and palaeontological evidence. Marine Collignon, Natural History Museum, University of Oslo, P.O. Box 1172 Blindern, NO-0318 Oslo, Norway. Present address: ETH Zürich, Geologisches Institut, Sonneggstrasse 5, NO E21, 8092 Zurich, Switzerland. E-mail: [email protected]. Øyvind Hammer, Natural History Museum, University of Oslo, P.O. Box 1172 Blindern, NO-0318 Oslo, Norway. E-mail: [email protected] Introduction most of the -
Stratigraphic and Geochemical Expression of Barremian–Aptian Global Climate Change in Arctic Svalbard
Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard Vickers, Madeleine; Price, Gregory D.; Jerrett, Rhodri; Watkinson, Matthew Published in: Geosphere DOI: 10.1130/GES01344.1 Publication date: 2016 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Vickers, M., Price, G. D., Jerrett, R., & Watkinson, M. (2016). Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard. Geosphere, 12(5), 1594-1605. https://doi.org/10.1130/GES01344.1 Download date: 03. okt.. 2021 Research Paper GEOSPHERE Stratigraphic and geochemical expression of Barremian–Aptian global climate change in Arctic Svalbard GEOSPHERE; v. 12, no. 5 Madeleine L. Vickers1, Gregory D. Price1, Rhodri M. Jerrett2, and Matthew Watkinson1 1School of Geography, Earth and Environmental Sciences, Plymouth University, Drake Circus, Plymouth, Devon PL4 8AA, UK doi:10.1130/GES01344.1 2School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Williamson Building, Oxford Road, Manchester M13 9PL, UK 5 figures; 2 supplemental files ABSTRACT island have been difficult, and precise, high-resolution dating of this succes- CORRESPONDENCE: madeleine .vickers@ plymouth sion has not been possible. This has meant that fully interpreting the conflict- .aca.uk Significant changes in global climate and carbon cycling occurred during the ing paleo climatic evidence from this Early Cretaceous succession has not been Early Cretaceous. This study examines the expression of such climatic events in possible in a global context; therefore, this paleo–high-latitude site has been of CITATION: Vickers, M.L., Price, G.D., Jerrett, R.M., and Watkinson, M., 2016, Stratigraphic and geo- high-latitude Svalbard together with the stratigraphic utility of carbon-isotope limited use for understanding Early Cretaceous global climate change. -
Paralic Sedimentation on an Epicontinental Ramp Shelf During a Full Cycle of Relative Sea-Level Fluctuation
NORWEGIAN JOURNAL OF GEOLOGY Paralic sedimentation on an epicontinental ramp shelf 343 Paralic sedimentation on an epicontinental ramp shelf during a full cycle of relative sea-level fluctuation; the Helvetiafjellet Formation in Nordenskiöld Land, Spitsbergen Ivar Midtkandal, Johan Petter Nystuen and Jenö Nagy Ivar Midtkandal, Johan Petter Nystuen & Jenö Nagy. Norwegian Journal of Geology, vol. 87, pp. 343-359.Trondheim 2007. ISSN 029-196X. A depositional model for the development of the Helvetiafjellet Formation in Nordenskiöld Land, Spitsbergen is presented. The formation was deposited into a segment of the large epicontinental Boreal basin that rimmed northern Pangaea during the Early Cretaceous. A wide range of depositional subenvironments are recorded within the succession; including fluvial braidplain, shallow marine bay, delta, coastal plain and fluvial channel. The depositional model approaches a layer-cake style for this part of the basin, caused by the rapid rates of progradation and retrograda- tion made possible by the gentle depositional gradient. An initial period of fluvial deposition arose in response to an early rise in relative sea-level. Following a regional flooding, the progradational to aggradational architecture in the area reflects a balanced rate of increase in accommodation vs. rate of sedimentation (A/S) ratio. This resulted in a heterolithic stacking of sandstone and mudstone. Autogenic variables are thought to have domi- nated the lateral facies variations recorded in the upper and middle parts of the succession. Ivar Midtkandal ([email protected]), Johan Petter Nystuen ([email protected],) Jenö Nagy ([email protected]). Department of Geoscien- ces, University of Oslo, P.O Box 1047 Blindern, NO-0316 Oslo Norway Introduction vial, tidal and wave-induced currents. -
The Jurassic and Cretaceous Sequence in Spitsbergen
The Jurassic and Cretaceous Sequence in Spitsbergen The Jurassic and Cretaceous sequence of Spitsbergen, Svalbard archipelago, is described and a revised lithostratigraphical scheme, of four formations, is proposed. The main episode of tectonic activity, together with dolerite intrusion, was in late Jurassic-early Cretaceous times and is represented by a non-sequence and local unconformity between the two lower formations. The fauna1 succession is also discussed. THEJurassic and Cretaceous rocks of Spitsbergen are exposed as an elliptical outcrop around the main Tertiary syncline (Text-fig. 1 ). Along the west coast the rocks have been folded and thrust in a deforma t'Ion belt of Tertiary age but in the north and east are gently dipping and little deformed, apart from local activity along fault belts. Jurassic fossils were first collected from Spitsbergen by Lovtn in 1837 from Grsnfjorden, and subsequent expeditions, led principally by Nordenskiold and Nathorst, established the presence of Jurassic and " Neocomian " strata along the south side of Isfjorden, in Bellsund, at Agardhbukta on the east coast, and on Kong Karls Land, the group of islands which lie some 150 km east of Vestspitsbergen. The results of these early expeditions were summarized by Nathorst (1910). Subsequent palaeontological work was based mainly on material from the Festningetl section (Hoel and Orvin, 1937; Sokolovand Bodylevsky, 1931 ; Frebold and Stoll, 1937) but much information on other localities and collections was given in a series of papers by Frebold (1929 a-c, 1930, 1931) who also discussed the palaeogeography and correlation of the Arctic Jurassic and Cretaceous rocks. Useful summaries of the Jurassic-Cretaceous sequence were given by Frebold in his two reviews of Spitsbergen geology (1935, 1951) and Arkell (1956) has, in particular, discussed the Jurassic faunas. -
The Tectonic and Sedimentary History of Svalbard
AG 209 The Tectonic and Sedimentary History of Svalbard Excursion Report August 2006 Søren H. Rasmussen Front picture: Pyramiden Mountain The Tectonic and Sedimentary History of Svalbard 2 Index 1. Introduction..................................................................................................................................4 2. Festningen ....................................................................................................................................5 3. Botnheia .....................................................................................................................................11 4. Janusfjellet .................................................................................................................................12 5. Helvetiafjellet Formation ...........................................................................................................14 6. Basilikafjellet .............................................................................................................................15 7. Storvola ......................................................................................................................................18 8. Pyramiden Mountain..................................................................................................................19 9. Billefjorden Basin ......................................................................................................................20 10. Lövehovden Mountainside.....................................................................................................22 -
Structural Development Along the Billefjorden Fault Zone in the Area Between Kjellstromdalen and Adventdalen/Sassendalen, Central Spitsbergen
Structural development along the Billefjorden Fault Zone in the area between Kjellstromdalen and Adventdalen/Sassendalen, central Spitsbergen PAL HAREMO, ARlLD ANDRESEN. HENNlNG DYPVlK, JENO NAGY, ANDERS ELVERH01, TOR ARNE EIKELAND AND HALVOR JOHANSEN Haremo, P.. Andresen, A., Dypvik. H., Nagy. J., Elvcrhsi. A,, Eikeland. T. A. 8: Johanscn, H. 1YW: Structural development along th? Billefjordcn Fault Zone in the area betwccn Kjellstriimdalen and Adventdalen/Sassendalen, central Spitsbergen. Polar Res. 8, 195-216. The Bilkfjorden Fault Zone represents a major lineament on Spitsbergen with a history of tectonic activity going back into the Devonian and possibly earlier. Recent structural, sedimentologicdl and stratigraphical investigations indicate that most of the stratigraphic thickness variations within the Mesozoic strata along thc Billefjordcn Fault Zone south of Isfjorden arc due to Tertiary compressional tectonics related to the transpressivc Eocenc West-Spitsbergen Orogcny. No convincing evidence of distinct Mesozoic cxtcnsional events. as suggested by previous workers. has been recognized. Tertiary compressional tcctonics are characterized by a combined thin-skinncd/thjck-skinnedstructural style. DCcollement zones arc recognized in the Triassic Sassendalen Group (Lower Decollement Zone) and in Ihc Jurassic/Crctaceous Janusfjcllct Subgroup (Upper DCcollcmcnt Zonc). East-vergent folding and reverse faulting associated with thcsc dicollement zones have resulted in the development of compressional structures. of which the major arc the Skolten and Tronfjcllct Anticlincs and the Adventelva Duplex. Movements on one or morc high angle east-dipping reverse faults in the pre-Mesozoic basement have resulted in the development of Ihc Juvdalskampen Monocline. and are responsible for out-of-scquenccthrusting and thinning of the Mesozoic sequence across the Bilkfjorden Fault Zone. -
Juha Matti Ahokas
Depositional Environment, Processes and Sequence Stratigraphy of the Paralic Helvetiafjellet Formation in Ullaberget, Southern Spitsbergen Juha Matti Ahokas Master of Science Thesis in Sedimentology and Petroleum Geology University of Oslo, Department of Geosciences June, 2004 2 Acknowledgements First of all I would like to thank my primary supervisor, Johan Petter Nystuen, who has helped and motivated me from the beginning. I would also like to thank Ron J. Steel and Erling Heinz Siggerud who initiated this project, provided working hypothesis and helped with the funding. The field work would not have been possible without help of the assistance of Liv Hege Lunde Birkeland and Ph.D project of Ivar Midtkandal. Big thanks for your time and patience. I would also like to thank all the people who have contributed with insights and feedback. I really appreciate that. I also would like to thank friends back in Department of Geology in the University of Turku, and especially give a big handshake to Jussi Hovikoski and Professor in sedimentology Matti Räsänen, for supporting the idea of taking Master thesis abroad. Jussi, start saving money for the jacket! And at last but not least I would like to thank Tiina for all the support! Oslo June 2004, Juha Matti Ahokas This manuscript was written in Microsoft Word, and figures were edited and made with Adobe Photoshop 6.0 and Adobe Illustrator 10.0. 4 Acknowledgements Table of contents I Abstract………………………………………………………………. 7 1 Introduction…………………………………………………………. 9 2 Field work and data………………………………………………… 11 2.1 Field work……………………………………………………………………... 11 2.2 Field data…………………………………………………………………...…. 13 3 Geological framework………………………………………………. -
Carboniferous–Permian) of South Spitsbergen
vol. 30, no. 3, pp. 193–230, 2009 doi: 10.4202/ppres.2009.10 Foraminifers from the Treskelodden Formation (Carboniferous–Permian) of south Spitsbergen Błażej BŁAŻEJOWSKI Instytut Paleobiologii PAN, Twarda 51/55, 00−818 Warszawa, Poland <[email protected] > Abstract: The organodetritic, sandy limestones of the Treskelodden Formation (Late Gzhelian to Early Artinskian) investigated in outcrops at Treskelen Peninsula, Hyrnefjellet mount and Polakkfjellet mount of south Spitsbergen, contain rich foraminiferal assem− blages. Fifty eight foraminiferal species of twenty three genera, including two new species (Hemigordius hyrnefjelleti sp. nov. and Midiella arctica sp. nov.) have been identified. Three foraminiferal zones have been defined, with ages of Late Asselian (Pseudofusulinella occidentalis), Sakmarian (Midiella ovata – Calcitornella heathi) and Early Artinskian (Hemigordius hyrnefjelleti – Midiella arctica). Sedimentary features and the biotic history of the studied succession records a Late Paleozoic cooling trend that stays in accordance with Pangaea’s shift to the north. Key words: Arctic, Svalbard, paleontology (foraminifers), biostratigraphy, Late Paleozoic. Introduction This paper documents the distribution of small foraminifers and fusulinaceans in three Upper Carboniferous–Lower Permian stratigraphic sections from south Spitsbergen. Late Paleozoic smaller foraminifers have received comparatively lit− tle attention in comparison with the fusulinaceans and do not figure prominently in correlation schemes. Sosipatrova (1967, 1969) presented the first stratigraphic scheme for the Upper Paleozoic deposits in the central Spitsbergen, and described many new species and genera of small foraminifers and fusulinaceans. The Polish Geological and Paleontological Spitsbergen Expeditions of 1957–1960 (Birken− majer 1964) and 1974–1979 (Biernat and Szymańska 1982) brought new material from south Spitsbergen, and the foraminifers were mentioned by Liszka (1964) and Peryt and Małkowski (1976). -
Gravel Fraction on the Spitsbergen Bank, NW Barents Shelf*
Gravel Fraction on the Spitsbergen Bank, NW Barents Shelf* MARC B. EDWARDS Edwards, M. B. 1975: Gravel fraction on the Spitsbergen Bank, NW Barents Shelf. Norges geol. Unders. 316, 205-217. The gravel fraction of the bottom sediment on the Spitsbergen Bank, located south of Svalbard in the NW Barents Sea, is composed predominantly of clastic sedimentary rocks, especially sandstone and shale. Between sampling stations the proportion of eight lithologic types is markedly different, ruling out the possibility of large-scale transport of the gravel by ice-rafting. Striated pebbles occur in small numbers: a few are exotic in composition, but most are similar to a non-striated rock-type at a given station. This suggests that the gravel was formed by reworking of previously deposited glacial material, which tends to be locally derived. The sandstone pebbles in the gravel include a variety of petrographic types, most of which are identical or similar to sandstones of known stratigraphic position on Svalbard. Observations on Mesozoic rocks on Bjørnøya, Hopen and southern Spitsbergen, and on the distribution of pebbles as described herein, suggest that the Spitsbergen Bank is underlain by nearly flat-lying Mesozoic sedimentary rocks similar to those known on Svalbard. The overall structure is a gentle syncline; a southward continuation of the dominant regional structure of Spitsbergen. Marc B. Edwards, Continental Shelf Division, Royal Norwegian Council for Scientific and Industrial Researcb; Norsk Polarinstitutt, N-1330 Oslo Lufthavn, Norway Introduction The Spitsbergen Bank is approximately 200 by 350 km, elongated NE-SW, lying south of Svalbard in the NW part of the Barents Sea (Fig. -
Lower Cretaceous Lithostratigraphy Across a Regional Subaerial Unconformity in Spitsbergen 287
NORWEGIAN JOURNAL OF GEOLOGY Lower Cretaceous lithostratigraphy across a regional subaerial unconformity in Spitsbergen 287 Lower Cretaceous lithostratigraphy across a regional subaerial unconformity in Spitsbergen: the Rurikfjellet and Helvetiafjellet formations Ivar Midtkandal, Johan Petter Nystuen, Jenö Nagy & Atle Mørk Midtkandal, I., Nystuen, J. P., Nagy, J. & Mørk, A.: Lower Cretaceous lithostratigraphy across a regional subaerial unconformity in Spitsbergen: the Rurikfjellet and Helvetiafjellet formations. Norwegian Journal of Geology, Vol. 88, pp. 287-304, Trondheim 2008, ISSN 029-196X During development of the Lower Cretaceous succession in the Spitsbergen domain of the epicontinental Boreal Basin, a fall in relative sea-level caused a major subaerial unconformity to form. This unconformity forms the lithostratigraphic boundary between the Rurikfjellet Formation below, and the Helvetiafjellet Formation above. The previous Ullaberget Member in the upper part of the Rurikfjellet Formation was originally defi- ned using the Ullaberget section in Nathorst Land as its stratotype. The Ullaberget section is not representative for the upper sandstone-rich mem- ber of the Rurikfjellet Formation, but is chosen here as the stratotype for the new Louiseberget Bed of the Festningen Member. The Louiseberget Bed consists of deltaic sandstone, located above the subaerial unconformity capping the Rurikfjellet Formation, and forms a facies body within the Festningen Member, the fluvially-dominated lower member of the Helvetiafjellet Formation. The Kikutodden Member is here defined as a new member substituting for the Ullaberget Member as the upper, sand-rich part of the Rurikfjellet Formation; the Kikutodden section in Sørkapp Land being the stratotype and the Strykejernet section being new hypostratotype for the member. The Festningen Member and the Glitrefjellet Member in the lower and upper parts of the Helvetiafjellet Formation, respectively, are re-established as formal members.