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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Development genes and evolution 197 (1988), S. 307-320 
    ISSN: 1432-041X
    Keywords: Parascaris ; Nematoda ; Chromatin diminution ; Cleavage pattern ; Local presomatic activation (LPA)
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary In Parascaris developmental commitment to the germ line and somatic lineages is indicated by the orientation of the mitotic spindle in blastomeres, the topology of cells in the embryo, and chromatin diminution in presomatic blastomeres. Using three different experimental techniques: transient pressure treatment, application of cytochalasin B, and isolation of blastomeres, we have succeeded in uncoupling several developmental processes during cleavage of P. univalens. The following results were obtained: (1) Following mitotic nondisjunction we observed identical behavior of all chromatids in each blastomere. Thus chromosome differentiation by differential replication does not occur. (2) Chromosome fragments obtained by pressure treatment of egg cells underwent chromatin diminution. Thus this process does not require an intact germ-line chromosome. However, chromosomes immobilized on a monopolar spindle did not undergo chromatin diminution. Thus diminution appears to require segregation of chromatids. (3) Blastomeres that completely lacked chromosomes as a result of mitotic nondisjunction underwent normal early cleavage divisions. (4) Pressure treatment or prolonged treatment with cytochalasin B caused egg cells or germ line blastomeres to lose their germ line quality, as deduced from the coincident occurrence of symmetrical (presomatic-like) cleavage and chromatin diminution. (5) Isolated blastomeres from 2-cell embryos, i.e. 1/2 blastomeres, usually cleaved according to their prospective fates in the whole embryo. However, in some partial embryos derived from such blastomeres, chromatin diminution was delayed for either one or two cleavage mitoses. An “activation” model as an alternative to a prelocalization model is presented, which can account for early blastomere topogenesis and chromatin diminution.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-07-13
    Description: We analyze daily wintertime cyclone variability in the central and eastern Mediterranean during 1958-2001, and identify four distinct cyclone states, corresponding to the presence or absence of cyclones in each basin. Each cyclone state is associated with wind flows that induce characteristic patterns of cooling via turbulent (sensible and latent) heat fluxes in the eastern Mediterranean basin and Aegean Sea. The relative frequency of occurrence of each state determines the heat loss from the Aegean Sea during that winter, with largest heat losses occurring when there is a storm in the eastern but not central Mediterranean (eNOTc), and the smallest occurring when there is a storm in the central but not eastern Mediterranean (cNOTe). Time series of daily cyclone states for each winter allow us to infer Aegean Sea cooling for winters prior to 1985, the earliest year for which we have daily heat flux observations. We show that cyclone states conducive to Aegean Sea convection occurred in 1991/1992 and 1992/1993, the winters during which deep water formation was observed in the Aegean Sea, and also during the mid-1970s and the winters of 1963/1964 and 1968/1969. We find that the eNOTc cyclone state is anticorrelated with the North Atlantic Oscillation (NAO) prior to 1977/1978. After 1977/1978, the cNOTe state is anticorrelated with both the NAO and the North Caspian Pattern (NCP), showing that the area of influence of large scale atmospheric teleconnections on regional cyclone activity shifted from the eastern to the central Mediterranean during the late 1970s. A trend toward more frequent occurrence of the positive phase of the NAO produced less frequent cNOTe states since the late 1970s, increasing the number of days with strong cooling of the Aegean Sea surface waters.
    Keywords: Earth Resources and Remote Sensing; Meteorology and Climatology
    Type: GSFC-E-DAA-TN11507 , Regional Environmental Change (ISSN 1436-3798); 14; 5; 1713-1723
    Format: application/pdf
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