0 10513 10521 10527 10531 10537 10539 10543 10549 10551 10557 10563 10567 10569 10573 10579 10581 10587 10591 10593 10597 10599 10603 10605 10607 10608 10609 10611 10612 10613 10615 10617 10621 10623 10627 10629 10633 10639 10641 10647 10651 10653 10657 10663 10669 10671 10677 10681 10683 10689 10693 10699 10707 11751 手机卡在我这 glacial-interglacial cycle lasts about 100,000 years (CLIMAP 1976), of which 90,000 years are rela- tively cold, and during which continental glaciers develop and expand at middle and high latitudes. Approximately 10,000 years of each climatic cycle are characterized by warm climate, for example the current, or Holocene, interglacial interval. The Quaternary Period is also defined on the basis of minimal evolution or extinction of both terrestrial and marine flora and fauna (Lye11 1834; Kurt& and Anderson 1980). Two major exceptions to this are He tried to profiteer from this dirty deal. 手术后没有感染 Born, just waiting for the death of the course detailed carton printing the evolution of Homo sapiens about 400,000 years ago (Bowen 1985) and the late-Quaternary extinc- tions of numerous species of megafauna, for exam- ple, occurring in North America at the end of the Pleistocene, 10,000 years ago (Martin and Klein 1984). For the late-Quaternary time interval, cor- responding to the most recent glacial-interglacial cycle, an absolute chronology of events is available through radiocarbon dating, an isotopic-dating’ technique useful to about 80,000 years Before Present (yr B.P.). The late Quaternary is character- ized by major changes in species distributions and composition of biotic communities; only during the Holocene interval have modern distributional ranges of the biota taken shape and contemporary biotic communities assembled (Kurten and Ander- son 1980; Davis 1981, 1983; Huntley and Birks 1983; Nilsson 1983; Graham 1986; Graham et al. 1987; Delcourt and Delcourt 1987a; Ritchie 1987). The Quaternary Period represents not only a por- tion of the history of life on earth, but it also in- cludes the present day and will extend into both the immediate and the distant future. Paleoecological studies that reconstruct late-Quaternary landscape changes (Berglund I986) thus can be designed to dovetail with other methods of ‘investigation, in- cluding historical records and shorter-term data sets, to integrate landscape patterns and processes on a nested series of temporal and spatial scales in ecological time. An appreciation of past changes in both environment and biota is imperative for evalu- ating the current trajectory of change in landscapes (Delcourt et al. 1983a; Jacobson and Grimm 1986; Clark 1986). Histories of landscape development that can be reconstructed using paleoecological techniques provide long-term ‘experiments of the past’ (‘natural experiments’ sense Diamond 1986) that give a basis for testing alternative hypotheses about the relative influences of environmental change, biological interactions, and human activi- ties in structuring biotic communities within land- scape mosaics (Delcourt and Delcourt 1987a, b). Changes in landscapes on a Quaternary time scale have been two-fold: (1) changes in climate and in geomorphic processes have affected vegetational patterns and processes on natural landscapes on the scale of hundreds of years to hundreds of thou- 纸张很便宜，而且很轻 According to factory comment, VF specification on this diode is less than 1.2V at IF=200MA. 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