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  • 1
    In: Paleoceanography, Hoboken, NJ : Wiley, 1986, 19(2004), 1944-9186
    In: volume:19
    In: year:2004
    In: extent:17
    Description / Table of Contents: An 8 million year record of subtropical and midlatitude shelf-sea temperatures, derived from oxygen isotopes of well-preserved brachiopods from a variety of European sections, demonstrates a long-term Cenomanian temperature rise (16-20°C, midlatitudes) that reached its maximum early in the late Turonian (23°C, midlatitudes). Superimposed on the long-term trend, shelf-sea temperatures vary at shorter timescales in relation to global carbon cycle perturbations. In the mid-Cenomanian and the late Turonian, two minor shelf-sea cooling events (2-3°C) coincide with carbon cycle perturbations and times of high-amplitude sea level falls. Although this evidence supports the hypothesis of potential glacioeustatic effects on Cretaceous sea level, the occurrence of minimum shelf-sea temperatures within transgressive beds argues for regional changes in shelf-sea circulation as the most plausible mechanism. The major carbon cycle event in the latest Cenomanian (oceanic anoxic event 2) is accompanied by a substantial increase in shelf-sea temperatures (4-5°C) that occurred ~150 kyr after the commencement of the Delta 13 C excursion and is related to the spread of oceanic conditions in western European shelf-sea basins. Our oxygen isotope record and published Delta 18 O data of pristinely preserved foraminifera allow the consideration of North Atlantic surface water properties in the Cenomanian along a transect from the tropics to the midlatitudes. On the basis of fossil-derived Delta 18 O, estimated Delta w ranges, and modeled salinities, temperature-salinity-density ranges were estimated for tropical, subtropical, and midlatitude surface waters. Accordingly, the Cenomanian temperate shelf-seas waters have potentially the highest surface water density and could have contributed to North Atlantic intermediate to deep waters in the preopening stage of the equatorial Atlantic gateway.
    Type of Medium: Online Resource
    Pages: 17 , graph. Darst
    ISSN: 1944-9186
    Language: English
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  • 2
    Keywords: Dissertation ; Western Interior Seaway ; Marine Sedimente ; Klimaveränderung ; Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 231 Bl., 15.33 MB) , Ill., graph. Darst., Kt.
    Language: English
    Note: Kiel, Univ., Diss., 2002
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  • 3
    Keywords: Dissertation ; Western Interior Seaway ; Marine Sedimente ; Klimaveränderung ; Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource ( 236Seiten = 11MB) , Ill., graph. Darst., Kt.
    Language: English
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  • 4
    Publication Date: 2018-09-24
    Type: Article , NonPeerReviewed
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  • 5
    Publication Date: 2012-07-06
    Description: Northeast Atlantic 2004 Cruise No. 61, Leg 1 April 19 to May 4, 2004, Lisbon – Cork
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
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    Kluwer Academic / Plenum Publishers
    In:  In: Geologic Modeling and Simulation: Sedimentary Systems. , ed. by Merriam, D. F. and Davis, J. C. Kluwer Academic / Plenum Publishers, New York, USA, pp. 153-167.
    Publication Date: 2018-02-06
    Type: Book chapter , NonPeerReviewed
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  • 7
    Publication Date: 2019-09-23
    Description: 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. The sediments indicate orbital control of climate, reflected in fluctuations in the clastic influx and variations in carbonate and organic matter production. Trace element concentrations in the Volgian-Berriasian sediments suggest that the central part of the Greenland-Norwegian Seaway might have had suboxic bottom water beneath an oxic water column. Both marine and terrigenous organic matter are present in the seaway sediments. The Volgian-Berriasian strata have unusually high contents of organic carbon and are the source rocks for petroleum and gas fields in the region. The accumulation of organic carbon is attributed to restricted conditions in the seaway during this time of low sea level. It might be that the Greenland-Norwegian segment was the deepest part of the transcontinental seaway, bounded at both ends by relatively shallow swells. The decline in organic matter content of the sediments in the Valanginian-Hauterivian indicates greater ventilation and more active flow through the seaway as the sea level rose. The same benthic foraminifera assemblages are encountered throughout the seaway. Endemic assemblages of arenaceous foraminifera in the Volgian-Berriasian give way to more diverse and cosmopolitan Valanginian-Hauterivian benthic communities that include calcareous species. The foraminiferal assemblages also suggest low oxygen content bottom waters during the earlier Cretaceous, changing to more fully oxygenated conditions later. The calcareous nannoplankton, particularly Crucibiscutum salebrosum, which is rare at low latitudes and abundant in high latitudes, reflect the meridional thermal gradient. They indicate that the Greenland-Norwegian segment of the seaway was north of a subtropical frontal zone that acted as a barrier between the Tethyan and Boreal Realms. This implies the existence of stable climatic belts during the early Valanginian and Hauterivian, significant meridional temperature gradients, and moderate “ice house” conditions.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2017-05-10
    Description: An 8 million year record of subtropical and midlatitude shelf-sea temperatures, derived from oxygen isotopes of well-preserved brachiopods from a variety of European sections, demonstrates a long-term Cenomanian temperature rise (16–20°C, midlatitudes) that reached its maximum early in the late Turonian (23°C, midlatitudes). Superimposed on the long-term trend, shelf-sea temperatures vary at shorter timescales in relation to global carbon cycle perturbations. In the mid-Cenomanian and the late Turonian, two minor shelf-sea cooling events (2–3°C) coincide with carbon cycle perturbations and times of high-amplitude sea level falls. Although this evidence supports the hypothesis of potential glacioeustatic effects on Cretaceous sea level, the occurrence of minimum shelf-sea temperatures within transgressive beds argues for regional changes in shelf-sea circulation as the most plausible mechanism. The major carbon cycle event in the latest Cenomanian (oceanic anoxic event 2) is accompanied by a substantial increase in shelf-sea temperatures (4–5°C) that occurred ∼150 kyr after the commencement of the δ13C excursion and is related to the spread of oceanic conditions in western European shelf-sea basins. Our oxygen isotope record and published δ18O data of pristinely preserved foraminifera allow the consideration of North Atlantic surface water properties in the Cenomanian along a transect from the tropics to the midlatitudes. On the basis of fossil-derived δ18O, estimated δw ranges, and modeled salinities, temperature-salinity-density ranges were estimated for tropical, subtropical, and midlatitude surface waters. Accordingly, the Cenomanian temperate shelf-seas waters have potentially the highest surface water density and could have contributed to North Atlantic intermediate to deep waters in the preopening stage of the equatorial Atlantic gateway.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2023-01-31
    Description: A multidisciplinary study of upper Cenomanian-lower Turonian strata of the late Cretaceous Western Interior Seaway explored possible mechanisms for the formation of cyclic bedding sequences seen in the Western Interior Seaway. Numerical climate modeling was used to investigate the sensitivity of the climate to changes of one of the Earth's orbital parameters, the precession of the equinoxes. One complete precessional cycle was simulated with four orbital runs; 1) northern spring equinox at perihelion, 2) northern winter solstice at perihelion, 3) northern fall equinox at perihelion, and 4) northern summer solstice at perihelion. The cyclic organization of limestone/shale couplets seen in the sedimentological record of the central part of the Western Interior Seaway can be interpreted as reflecting climatic cycles. The most important mechanism for the formation of bedding couplets were changes induced by the precession of the equinoxes. The most important variable was surface runoff, which affected both the discharge of rivers and the amount of sediment transported into the Western Interior Seaway. Annual river discharge from western North America into the seaway was equivalent to a layer of fresh water ~0.3m thick. River discharge into the Arctic Ocean was even greater, equivalent to a layer more than 1m thick each year. These very large supplies of fresh water from land were adequate to maintain low salinity surface waters in the Arctic Ocean and the Western Interior Seaway. High surface runoff from the highlands bordering the Western Interior Seaway to the west occured during summer in three of the orbital configurations but low surface runoff when northern hemisphere winter is at perihelion. The precession signal seen in the sediment is interpreted as being produced by the elimination of high summer surface runoff when perihelion occurs during northern hemisphere winter.
    Type: Thesis , NonPeerReviewed
    Format: text
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