This paper deals with a new integrated method of reconstruction and forecasting of climatic changes in future. The method is based on proxy data pollen-spore analysis method, 14C analysis method, nowadays meteorologic...This paper deals with a new integrated method of reconstruction and forecasting of climatic changes in future. The method is based on proxy data pollen-spore analysis method, 14C analysis method, nowadays meteorological data, and data about of solar activity expressed in numbers of W （Wolf）. Here we present the results of investigation of sediments of the 2nd Fomich River terrace, Taymyr Peninsula, Russia. The formation of the peat bog started 10500 ± 140 years BP and continued during the entire Holocene. The pollen analysis of the sediment samples of the 2nd Fomich River terrace and the analysis of surface samples from a larch forest, typical of this region, reveals two phytochrones： both climatically preconditioned--tundra phytochrone （I1-4） and forest phytochrone （Ⅱ1-4）. The techniques of reconstruction and forecasting of basic elements of climate are presented and discussed in details.展开更多
Wolf＇s postherpetic isotopic response （PHIR） describes the occurrence of a new lesion at the site of a healed herpetic lesion. It is more commonly seen alter infection by varicella-zoster virus （VZV） than herpes ...Wolf＇s postherpetic isotopic response （PHIR） describes the occurrence of a new lesion at the site of a healed herpetic lesion. It is more commonly seen alter infection by varicella-zoster virus （VZV） than herpes simplex virus. Such postherpetic lesions present with a board spectrum from inflammatory diseases to malignancies.展开更多
文摘This paper deals with a new integrated method of reconstruction and forecasting of climatic changes in future. The method is based on proxy data pollen-spore analysis method, 14C analysis method, nowadays meteorological data, and data about of solar activity expressed in numbers of W （Wolf）. Here we present the results of investigation of sediments of the 2nd Fomich River terrace, Taymyr Peninsula, Russia. The formation of the peat bog started 10500 ± 140 years BP and continued during the entire Holocene. The pollen analysis of the sediment samples of the 2nd Fomich River terrace and the analysis of surface samples from a larch forest, typical of this region, reveals two phytochrones： both climatically preconditioned--tundra phytochrone （I1-4） and forest phytochrone （Ⅱ1-4）. The techniques of reconstruction and forecasting of basic elements of climate are presented and discussed in details.
基金This work is Supported by a grant from the National Natural Science Foundation of China （No. 81572671 ）.
文摘Wolf＇s postherpetic isotopic response （PHIR） describes the occurrence of a new lesion at the site of a healed herpetic lesion. It is more commonly seen alter infection by varicella-zoster virus （VZV） than herpes simplex virus. Such postherpetic lesions present with a board spectrum from inflammatory diseases to malignancies.
