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  • 1
    Type of Medium: Book
    Pages: 112 S
    Language: Undetermined
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 7 (1987), S. 163-171 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Sea-ice microflora was collected from December 1971 to November 1972 from a variety of types of sea ice in the vicinity of Arthur Harbor, Anvers Island, Antarctic Peninsula. Sixty-seven identifiable species of diatoms, one silicoflagellate and several archaeomonads were recoverd from the ice. Of these, only 24 diatoms and the archaeomonads were considered to be truly cryophilic based on their occurrence and abundance. Qmode factor analysis revealed that four factors (species occurrences) account for 89% of the data. In a general way, these four factors are related to ice type-shore ice protected from turbulence, grounded pack ice, slush ice and sea ice. Shannon-Wiener species diversity functions range from 0.000 (monospecific) to 3.0515 (dominance divided among 9 species). Diversity also appeared to be related to ice type-protected shore ice was low, sea ice was intermediate, and grounded pack, exposed shore ice and slush were higherst. Short-term varibility in physical/biotic environment may control species diversity. Sea-ice assemblages may be useful in paleoclimatic interpretations of past ice distributions.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In an area north-east of our site, at 14N and 117W, Johnson1 found that siliceous microfossil preservation was excellent in the surface sediments but deteriorated markedly 1-2 m below the sea floor, where biogenic opal was totally absent. Coincident with this disappearance of biogenic opal, there ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 287 (1980), S. 725-726 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Figure 1 shows the results of the 230Th dating of the nodule; these are consistent with growth rates found by others using this method for other nodules3'5. The nodule's top 3 mm indicate a growth rate of 3 mm Myr"1, and the bottom yielded a rate of 4.5 mm Myr l. (The bottom result is only an ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1573-5117
    Keywords: North Atlantic ; surface sediments ; diatom abundance
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Valve abundances of marine planktonic, marine benthic and freshwater diatoms in 780 sediment surface samples from the North and Equatorial Atlantic between 20° S 75° W and 70° N 10° E display patterns that do not correspond to published records of primary production in the photic zone. On the contrary, their abundance is more closely related to dissolution and dilution by terrigenous minerogenic and biogenic carbonate material. Highest abundances of marine planktonic diatoms occur in the northern North Atlantic south of Iceland and in the equatorial regions. The central North Atlantic and the central Caribbean, which feature lower primary production in the photic zone, contain few or no diatoms in surface sediments. African derived freshwater diatoms are concentrated in a lobe between 5° S and 20° N latitude decreasing in numbers from the African continent westward.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Geology 255 (2008): 64-82, doi:10.1016/j.margeo.2008.07.005.
    Description: During the late glacial, marine isotope Stage 2, the Marmara Sea transformed into a brackish lake as global sea level fell below the sill in the Dardanelles Strait. A record of the basin’s reconnection to the global ocean is preserved in its sediments permitting the extraction of the paleoceanographic and paleoclimatic history of the region. The goal of this study is to develop a high-resolution record of the lacustrine to marine transition of Marmara Sea in order to reconstruct regional and global climatic events at 24 a millennial scale. For this purpose, we mapped the paleoshorelines of Marmara Sea along the northern, eastern, and southern shelves at Çekmece, Prince Islands, and Imrali, using data from multibeam bathymetry, high-resolution subbottom profiling (chirp) and ten sediment cores. Detailed sedimentologic, biostratigraphic (foraminifers, mollusk, diatoms), X-ray fluorescence geochemical scanning, and oxygen and carbon stable isotope analyses correlated to a calibrated radiocarbon chronology provided evidence for cold and dry conditions prior to 15 ka BP, warm conditions of the Bolling-Allerod from ~15 to 13 ka BP, a rapid marine incursion at 12 ka BP, still stand of Marmara Sea and sediment reworking of the paleoshorelines during the Younger Dryas at ~11.5 to 10.5 ka BP, and development of strong stratification and influx of nutrients as Black Sea waters spilled into Marmara Sea at 9.2 ka BP. Stable environmental conditions developed in Marmara Sea after 6.0 ka BP as sea-level reached its present shoreline and the basin floors filled with sediments achieving their present configuration.
    Description: Support for the analyses was from NSF-OCE-0222139; OCE-9807266 and PSC-CUNY 69138-00 38.
    Keywords: Late Pleistocene-Holocene ; Marmara Sea ; Sea-level ; Paleoshorelines ; Black Sea ; Mediterranean Sea
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 7
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 24 (2009): PA2214, doi:10.1029/2008PA001693.
    Description: The silicic acid leakage hypothesis (SALH) predicts that during glacial periods excess silicic acid was transported from the Southern Ocean to lower latitudes, which favored diatom production over coccolithophorid production and caused a drawdown of atmospheric CO2. Downcore records of 230Th-normalized opal (biogenic silica) fluxes from 31 cores in the Pacific sector of the Southern Ocean were used to compare diatom productivity during the last glacial period to that of the Holocene and to examine the evidence for increased glacial Si export to the tropics. Average glacial opal fluxes south of the modern Antarctic Polar Front (APF) were less than during the Holocene, while average glacial opal fluxes north of the APF were greater than during the Holocene. However, the magnitude of the increase north of the APF was not enough to offset decreased fluxes to the south, resulting in a decrease in opal burial in the Pacific sector of the Southern Ocean during the last glacial period, equivalent to approximately 15 Gt opal ka−1. This is consistent with the work of Chase et al. (2003a), and satisfies the primary requirement of the SALH, assuming that the upwelled supply of Si was approximately equivalent during the Holocene and the glacial period. However, previous results from the equatorial oceans are inconsistent with the other predictions of the SALH, namely that either the Corg:CaCO3 ratio or the rate of opal burial should have increased during glacial periods. We compare the magnitudes of changes in the Southern Ocean and the tropics and suggest that Si escaping the glacial Southern Ocean must have had an alternate destination, possibly the continental margins. There is currently insufficient data to test this hypothesis, but the existence of this sink and its potential impact on glacial pCO2 remain interesting topics for future study.
    Description: Funding for this research was provided in part by the U.S. NSF (grant OPP02-30268). We thank the core repository at LDEO and the Antarctic Research Facility at FSU for providing samples.
    Keywords: Southern Ocean ; Silica cycles ; Paleoceanography
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: image/jpeg
    Format: text/plain
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  • 8
    Publication Date: 2023-06-27
    Keywords: 86-576; Deep Sea Drilling Project; Demagnetization step; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg86; North Pacific; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; NRM, Intensity after demagnetization; Sample code/label; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 6077 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: 86-576B; Deep Sea Drilling Project; Demagnetization step; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg86; North Pacific; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; NRM, Intensity after demagnetization; Sample code/label; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 3295 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: 86-578; Deep Sea Drilling Project; Demagnetization step; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg86; North Pacific; NRM, Intensity after demagnetization; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 699 data points
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