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  • 1
    Type of Medium: Book
    Pages: 117 S , graph. Darst., Kt
    Series Statement: Berichte zur Polarforschung
    Language: German , English
    Note: Zugl.: Kiel, Univ., Diss, 1998
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  • 2
    Keywords: Dissertation ; Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource ( 173Seiten = 11MB) , graph. Darst., Kt
    Language: German
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  • 3
    Type of Medium: Book
    Pages: 52 S. , Ill., graph. Darst
    ISBN: 9789279052668
    Series Statement: EUR 22812 : EN
    Language: English
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  • 4
    Publication Date: 2020-12-21
    Description: This study presents the results of high-resolution sedimentological and clay mineralogical investigations on sediments from ODP Sites 908A and 909A/C located in the central Fram Strait. The objective was to reconstruct the paleo-climate and paleo-oceanography of the high northern latitudes since the middle Miocene. The sediments are characterised in particular by a distinctive input of ice-rafted material, which most probably occurs since 6 Ma and very likely since 15 Ma. A change in the source area at 11.2 Ma is clearly marked by variations within clay rnineral composition and increasing accumulation rates. This is interpreted as a result of an increase in water mass exchange through the Fram Strait. A further period of increasing exchange between 4-3 Ma is identified by granulometric investigations and points to a synchronous intensification of deep water production in the North Atlantic during this time interval. A comparison of the components of coarse and clay fraction clearly shows that both are not delivered by the same transport process. The input of the clay fraction can be related to transport mechanisms through sea ice and glaciers and very likely also through oceanic currents. A reconstruction of source areas for clay minerals is possible only with some restrictions. High smectite contents in middle and late Miocene sediments indicate a background signal produced by soil forrnation together with sediment input, possibly originating from the Greenland­Scotland Ridge. The applicability of clay mineral distribution as a climate proxy for the high northern latitudes can be confirrned. Based on a comparison of sedirnents from Site 909C, characterised by the smectite/illite and chlorite ratio, with regional and global clirnatic records (oxygen isotopes), a middle Miocene cooling phase between 14.8-14.6 Ma can be proposed. A further cooling phase between 10-9 Ma clearly shows similarities in its progress toward drastic decrease in carbonate sedimentation and preservation in the eastern equatorial Pacific. The modification in sea water and atmosphere chemistry may represent a possible link due to the built up of equatorial carbonate platforms. Between 4.8-4.6 Ma clay mineral distribution indicates a distinct cooling trend in the Fram Strait region. This is not accompanied by relevant glaciation, which would otherwise be indicated by the coarse fraction. The intensification of glaciation in the northern hernisphere is distinctly documented by a rapid increase of illite and chlorite starting from 3.3 Ma, which corresponds to oxygen isotope data trends from North Atlantic.
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 5
    Publication Date: 2019-07-01
    Description: DSDP/ODP drilling in the northern North Atlantic reveals that so far the onset of northern hemisphere cooling deduced from the occurrence of ice-rafted debris (IRD) in deep-sea sediments can be traced back to the middle Miocene. The Greenland ice sheet has probably the longest history on the northern hemisphere. Leg 151 site 909 (Fram Strait) recovered a unique continuous sediment record dating from early/middle Miocene. The composition of the coarse fraction indicates that the oldest IRD pulses are documented around 14 Ma in the Fram Strait (site 909) and around 12.6 Ma on the Vöring Plateau (leg 104, site 642) in the Norwegian–Greenland Sea. Fram Strait site 909 indicates a further stepwise increase of northern hemisphere cooling by serveral IRD pulses during late Miocene (between 10.8 and 8.6 Ma, around 7.2, 6.8 and 6.3 Ma), which ultimately led to a drastic intensification of northern hemisphere glaciation during Plio–Pleistocene. The deep-sea sediment records show that Plio–Pleistocene strengthening of IRD pulses have been observed since approximately 4.0 Ma in the westernmost Norwegian–Greenland Sea and Labrador Sea; by contrast, strengthening of IRD pulses are observed at approximately 3.2–2.7 Ma on the eastern side of the Norwegian–Greenland Sea, including the Barents Sea margin. Sediment composition and physical properties of the drilled, mostly terrigenous sections reveal that orbital parameters have controlled major aspects of shallow and deep-water environments with frequency domains related to 41 ka periods of obliquity dominant in the pre-glacial Miocene, Pliocene and early Quaternary and to 100 ka periods of eccentricity dominant during the past 600,000–700,000 years. The stratigraphy of ice-rafted material reveals a frequently and rapidly changing history of the dynamics of various segments in ice sheets around the Norwegian–Greenland Sea. It is particularly evident from the composition of the ice-rafted material that the Eurasian ice sheets delivered IRD to the eastern part of the Norwegian–Greenland Sea, whereas Greenland source areas are represented in the drill sites of the east Greenland continental margin and in the Labrador Sea. The stratigraphic sequences on the Yermak Plateau suggest that the Svalbard ice sheet may have extended far to the north prior to oxygen isope stage 16 but not since then. Invasions of temperate Atlantic waters during interglacials can be observed as short-lived and rather irregular events. It never reached the area off eastern Greenland except during the Pliocene interval, when tundra floras were able to develop on north-eastern Greenland and planktonic foraminifers suggesting the presence of temperate water masses in the Fram Strait as been documented in the drill sites from the Yermak Plateau.
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    PANGAEA
    In:  Supplement to: Winkler, Amelie (1999): Die Klimageschichte der hohen nördlichen Breiten seit dem mittleren Miozän: Hinweise aus sedimentologischen-tonmineralogischen Analysen (ODP Leg 151, zentrale Framstraße) (The climate history of the high northern latitudes since the Middle Miocene: indications from sedimentological and clay mineralogical analyses (ODP Leg 151, central Fram Strait)). Berichte zur Polarforschung = Reports on Polar Research, 344, 117 pp, https://doi.org/10.2312/BzP_0344_1999
    Publication Date: 2024-01-09
    Description: This study presents the results of high-resolution sedimentological and clay mineralogical investigations on sediments from ODP Sites 908A and 909AlC located in the central Fram Strait. The objective was to reconstruct the paleoclimate and paleoceanography of the high northern latitudes since the middle Miocene. The sediments are characterised in particular by a distinctive input of ice-rafted material, which most probably occurs since 6 Ma and very likely since 15 Ma. A change in the source area at 1 1.2 Ma is clearly marked by variations within clay mineral composition and increasing accumulation rates. This is interpreted as a result of an increase in water mass exchange through the Fram Strait. A further period of increasing exchange between 4-3 Ma is identified by granulometric investigations and points to a synchronous intensification of deep water production in the North Atlantic during this time interval. A comparison of the components of coarse and clay fraction clearly shows that both are not delivered by the Same transport process. The input of the clay fraction can be related to transport mechanisms through sea ice and glaciers and very likely also through oceanic currents. A reconstruction of source areas for clay minerals is possible only with some restrictions. High smectite contents in middle and late Miocene sediments indicate a background signal produced by soil formation together with sediment input, possibly originating from the Greenland- Scotland Ridge. The applicability of clay mineral distribution as a climate proxy for the high northern latitudes can be confirmed. Based on a comparison of sediments from Site 909C, characterised by the smectite/illite and chlorite ratio, with regional and global climatic records (oxygen isotopes), a middle Miocene cooling phase between 14.8-14.6 Ma can be proposed. A further cooling phase between 10-9 Ma clearly shows similarities in its Progress toward drastic decrease in carbonate sedimentation and preservation in the eastern equatorial Pacific. The modification in sea water and atmosphere chemistry may represent a possible link due to the built-up of equatorial carbonate platforms. Between 4.8-4.6 Ma clay mineral distribution indicates a distinct cooling trend in the Fram Strait region. This is not accompanied by relevant glaciation, which would otherwise be indicated by the coarse fraction. The intensification of glaciation in the northern hemisphere is distinctly documented by a rapid increase of illite and chlorite starting from 3.3 Ma, which corresponds to oxygen isotope data trends from North Atlantic.
    Keywords: 151-908; 151-908A; 151-909; 151-909A; 151-909C; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg151; North Greenland Sea; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 11 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Pflaumann, Uwe; Sarnthein, Michael; Ficken, Katherine; Grothmann, Alexandra; Winkler, Amelie (1998): Variations in eolian and carbonate sedimentation, sea surface temperature, and productivity off N.W. Africa over the last 3 M.Y. at Site 958 off Northwest Africa. In: Firth, JV (ed.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 159T, 3-16, https://doi.org/10.2973/odp.proc.sr.159T.061.1998
    Publication Date: 2024-01-09
    Description: Site 958 was drilled to monitor the late Neogene history of both continental aridity in northwestern Africa and the Canary Current distant from nearshore upwelling. Based on magnetostratigraphy, biostratigraphic datums, variations in carbonate, coarse fraction components, and the species composition of planktonic foraminifers, as well as using the d18O records of Globigerinoides ruber (white), we established a splice between Holes 958A and 958B and a stratigraphic age scale deciphering Milankovitch cycles. Over the last 630 k.y., sedimentation rates amount to 2.9 cm/k.y., and to 2.05-2.53 cm/k.y. back to the base of the Pleistocene. Extremely low rates of 0.4 cm/k.y. and a reworking of fossils mark the late Pliocene. The first continuous, long, sea-surface temperature (SST) record from the center of the Canary Current, which is based on foraminifer species census data, depicts a general temperature decrease in the late Pliocene, lower SST and high seasonalities of up to 6°C ~2.0-1.6 Ma, a warmer interval from 1.6 Ma to ~0.85 Ma, again lower SST and higher seasonalities until 0.33 or 0.26 Ma, and a final warmer interval, lasting until at least 50 ka, possibly reflecting the attenuated dynamics of the Canary Current. Especially over the last 400 k.y., since Stage 11, glacial stages are hardly reflected by cold SST cycles, except for various abrupt and extremely short cooling events amounting to D6°C, which possibly result from North Atlantic Heinrich events. Similar, but not necessarily synchronous, events of short-term, extremely high values occur in the paleoproductivity and (d13Cbased) paleonutrient records, which indicate a generally low primary production averaging to 180 g C m**-2 yr**-1 at 50-330 ka and about 300 g C m**-2 yr**-1 back to the base of the Pleistocene. Near 1.2-1.6 Ma, the grain-size and magnetic susceptibility records document a significant increase in the discharge of south Saharan/Sahelian dust, possibly linked to increasing aridity.
    Keywords: 159-958; 159-958A; Canarias Sea; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg159T; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 8
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    PANGAEA
    In:  Supplement to: Winkler, Amelie; Dullo, Wolf-Christian (2002): Data report: Miocene to Pleistocene sedimentation pattern on the Chatham Rise, New Zealand. In: Richter, C (ed.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 181, 1-21, https://doi.org/10.2973/odp.proc.sr.181.206.2002
    Publication Date: 2024-01-09
    Description: Site 1123 is located on the northeastern flank of the Chatham Rise. Sedimentological and clay mineralogical analyses indicate a very fine grained carbonate-rich sediment. Smectite and illite are the main constituents of the clay mineral assemblage. High smectite values in the Eocene decrease in younger sediment sequences. Illite and chlorite concentrations increase in younger sediments with significant steps at 13.5, 9, and 6.4 Ma. The kaolinite content is near the detection limit and not significant. We observed only small fluctuations of the clay mineral composition, which indicates a uniform sedimentation process, probably driven by long-term processes. Good correspondence is shown between increasing illite and chlorite values and the tectonic uplift history of the Southern Alps.
    Keywords: 181-1123; COMPCORE; Composite Core; Joides Resolution; Leg181; Ocean Drilling Program; ODP; South Pacific Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
    Publication Date: 2024-01-09
    Keywords: 181-1123; Accumulation rate, mass; AGE; Calcium carbonate; Calculated; Carbon, organic, total; COMPCORE; Composite Core; Depth, reference; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Element analyser CS, LECO; Joides Resolution; Leg181; Ocean Drilling Program; ODP; Sample code/label; Sample comment; Size fraction 〉 0.063 mm, sand; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 2590 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 181-1123; AGE; Calculated; Chlorite; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Illite; Joides Resolution; Kaolinite; Leg181; Ocean Drilling Program; ODP; Ratio; Sample code/label; Smectite; South Pacific Ocean; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 720 data points
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