Two-factor analysis of variance and redundancy analysis were used to analyze the characte-ristics of soil organic carbon total nitrogen storage in garden land,forestland,grassland,farmland,and bare land in the Dachunh...Two-factor analysis of variance and redundancy analysis were used to analyze the characte-ristics of soil organic carbon total nitrogen storage in garden land,forestland,grassland,farmland,and bare land in the Dachunhe watershed of Jinning District,Kunming City,Yunnan Province,China.The effects of the soil organic carbon,total nitrogen stratification ratio,soil physical and chemical factors on the storage characteristics of organic carbon and total nitrogen of different land-use types were analyzed.The results show that the rates of carbon and nitrogen stratification in soil from 0-20 cm and 40-60 cm of the same land-use types differed are statistically significant(P<0.05).The organic carbon and total nitrogen stratification ratio SR1 of garden land soil are 38.5%and 25.3%,respectively,which are higher than SR^(2).The soil organic carbon and total nitrogen stratification ratio SR^(2) of different land-use types are greater than SR1.There are statistically significant differences in the SR^(2) soil organic carbon and total nitrogen stratification ratios(P<0.05).Soil organic carbon and total nitrogen storage of diffe-rent land-use types gradually decrease with increasing soil depth,with the maximum soil organic carbon and total nitrogen storage in the 0-20 cm soil layer.Soil organic carbon and total nitrogen sto-rage at the same soil depth are significantly different(P<0.05).Soil organic carbon and total nitrogen storage in the garden land are greater than those in the other land-use types.Soil organic carbon and total nitrogen storage in 0-20 cm garden land are 4.96 and 3.19 times than those in bare land,respectively;soil organic carbon and total nitrogen storage are explained by 93.66%and 1.53%in redundancy analysis RDA1 and RDA2,respectively.All physicochemical factors except Available Phosphorus and pH are statistically significance with carbon and nitrogen storage(P<0.05).Soil cationic exchange capacity,Available Phosphorus,C/N ratio,and Moisture Content are positively correlated with organic carbon and total nitrogen storage.In contrast,soil Bulk Density is negatively correlated with organic carbon storage and total nitrogen storage.Available Phosphorus,C/N ratio,and Moisture Content are the main factors promoting soil organic carbon and total nitrogen accumulation.展开更多
The Cenozoic strata are well developed in the northwest of Yunnan Province, where the eastern boundary of Qing—Zang (Qinghai—Xizang) plateau is located. The rich geo\|records in the Cenozoic strata can help us to re...The Cenozoic strata are well developed in the northwest of Yunnan Province, where the eastern boundary of Qing—Zang (Qinghai—Xizang) plateau is located. The rich geo\|records in the Cenozoic strata can help us to recapitulate the evolution history of Qing—Zang plateau.1\ The Cenozoic Strata Ninglang Formation (Paleocene—Middle Eocene) is composed of massively bedded conglomerate , mudstone in the lower part, purple thinly bedded—medium bedded fine quartz sandstone and sandy shale in the upper part, 600m thick. Lijiang Formation (Upper Eocene) and Jinsichang Formation (Oligocene): conglomerate, with a little sandstone in lower part, claystone, with a little conglomerate in the upper part. Lijiang Formation unconformably overlies on Ninglang Formation or even older strata, 1500～2000m thick. Shuanghe Formation (Miocene): thinly—massively bedded muddy siltstone, fine sandstone, marl, with several layers of coal. It unconformably overlies on Jinsichang Formation or even older strata, 108m thick. Sanying Formation (Pliocene): Claystone, siltstone, with a little lignite in the middle and upper part, conglomerate at the base, 110m thick, widely spread in the northwest of Yunnan.Sheshan Formation (early Pleistocene): pebbles, sands and clay layers. It unconformably overlies on the older strata, 100～187m thick.Heyunsi Formation (middle Pleistocene): poorly sorted and poorly rounded gravel and sands, 100～347m thick.Upper Pleistocene Series: glaciers—gravel, sands and clays; alluvial—sandy gravel layer(terraces); lacustrine—fine sand, silt and clay layer, 100 m thick.Holocene Series: lacustrine—sand, silt and clay layers; alluvial—sandy gravel layer (terraces), 50m thick.展开更多
The southeast margin of Tibet plateau mainly consists of the Western Yunnan plateau (WYP). The uplift and denudation at the southeast margin of Tibet plateau can be represented by that of the WYP. Based on the uplift ...The southeast margin of Tibet plateau mainly consists of the Western Yunnan plateau (WYP). The uplift and denudation at the southeast margin of Tibet plateau can be represented by that of the WYP. Based on the uplift of ancient plantain surface, river terrace and sedimentary response in peripheral basins of the WYP, suggest that the WYP experienced a rapid uplift and denudation in Quaternary. The WYP have been uplifted about 610～700m, and eroded away about 1095～1600m since Quaternary, average denudation rate reach 0 68～0 94mm/a. Uplift rates in different time interval were calculated according to river terrace. Relations between WYP and Tibetan plateau are discussed further..The Yinggehai basin located at the south termination of the Red River fault, it is the younger (mainly Neogene) pull\|apart basin, which developed at releasing bend of the Red River right\|lateral wrench fault. Since the Neogene, the subsidence center of the Yinggehai basin shifted southward and, connected with the Southeast Hainan basin. Both basins collected large amounts of the Holocene and Quaternary deposits of marine origin. They are peripheral marine basin of the WYP.. Silicate clastic sediments in both basins have been large supported from the WYP into both basins through the Red River system. The total volumes derived from the WYP in the Neogene and Quaternary is 2 8004×10 14 t(1 and 5 1206×10 14 t. The sedimentation rate in Yinggehai basin rose from 0 52mm/a in the Neogene to 1 39mm/a in the Quaternary. The facts that accumulation volume and sedimentation rate rose greatly after the Neogene, suggested a rapid uplift in the WYP. The rapid uplift was responsible for the unconformity between the Neogene and Quaternary. Elevation of ancient planation surface,and river terrace supported the rapid uplift of the WYP also. The ancient planation surface was elevated from 2500～2600m to 3000～3200m during Quaternary, seven terraces in Tue can be traced through the field area in elevation from 20 5m to 612m above the modern river surface in the Lancang River. The Jinsha River also incised into bed rocks about 700m in Shigu. All the facts suggest that southeast margin of Tibet plateau rose rapidly; the plateau was elevated about 610～700m in the Quaternary.展开更多
In south\|eastern margin of Tibetan plateau, the Western Yunnan area of China, the NNW\|striking faults are dominant active structures. Their dextral strike\|slips cause conjugate slips along NE\|striking faults, and ...In south\|eastern margin of Tibetan plateau, the Western Yunnan area of China, the NNW\|striking faults are dominant active structures. Their dextral strike\|slips cause conjugate slips along NE\|striking faults, and these left shears induce blocks’ clockwise rotations along vertical axes. For example, Simao Block in the south part of Western Yunnan is bounded by Red River Fault (east), Lancang—Gengma Fault (west), Nandinghe Fault (north), and Dian Bien Phu Fault (south); and the right shears of Red River Fault and Lancang—Gengma Fault induced conjugate left shear along Nandinghe Fault and Dian Bien Phu Fault, and laters’ sinistral slips caused clockwise rotation of the Block. This rotation has been proved by geodetic measurements (Jiang, et al., 1993) and palaeomagnetic measurement (Wu, et al., 1987). In Pu’er area, which is located in the central part of Simao Block, several small\|scale blocks are clockwise rotated by sinistral shears of NE\|striking faults (Wang Yang, 1996). Block rotation along vertical axis is main active deformation style in Western Yunnan.展开更多
基金Natural Science Foundation of China(51979134,51779113)Yunnan Provincial Education Department Scientific Research Fund Project(2021J0164)+4 种基金Open Fund Project of Yunnan Provincial Key Laboratory of Highland Wetland Protection and Restoration and Ecological Services(202105AG070002)Provincial Innovation Team on Environmental Pollution and Food Safety and Human Health,Southwest Forestry University(2005AE160017)A Study of Terrestrial Animal Habitats in Li Ziping National Nature Reserve,Sichuan Province(2021ZD0125)The Construction Project of Key Disciplines with Advantages and Characteristics(Ecology)in Yunnan UniversitiesResearch Project of Key Laboratory of Soil Erosion and Control in Yunnan University。
文摘Two-factor analysis of variance and redundancy analysis were used to analyze the characte-ristics of soil organic carbon total nitrogen storage in garden land,forestland,grassland,farmland,and bare land in the Dachunhe watershed of Jinning District,Kunming City,Yunnan Province,China.The effects of the soil organic carbon,total nitrogen stratification ratio,soil physical and chemical factors on the storage characteristics of organic carbon and total nitrogen of different land-use types were analyzed.The results show that the rates of carbon and nitrogen stratification in soil from 0-20 cm and 40-60 cm of the same land-use types differed are statistically significant(P<0.05).The organic carbon and total nitrogen stratification ratio SR1 of garden land soil are 38.5%and 25.3%,respectively,which are higher than SR^(2).The soil organic carbon and total nitrogen stratification ratio SR^(2) of different land-use types are greater than SR1.There are statistically significant differences in the SR^(2) soil organic carbon and total nitrogen stratification ratios(P<0.05).Soil organic carbon and total nitrogen storage of diffe-rent land-use types gradually decrease with increasing soil depth,with the maximum soil organic carbon and total nitrogen storage in the 0-20 cm soil layer.Soil organic carbon and total nitrogen sto-rage at the same soil depth are significantly different(P<0.05).Soil organic carbon and total nitrogen storage in the garden land are greater than those in the other land-use types.Soil organic carbon and total nitrogen storage in 0-20 cm garden land are 4.96 and 3.19 times than those in bare land,respectively;soil organic carbon and total nitrogen storage are explained by 93.66%and 1.53%in redundancy analysis RDA1 and RDA2,respectively.All physicochemical factors except Available Phosphorus and pH are statistically significance with carbon and nitrogen storage(P<0.05).Soil cationic exchange capacity,Available Phosphorus,C/N ratio,and Moisture Content are positively correlated with organic carbon and total nitrogen storage.In contrast,soil Bulk Density is negatively correlated with organic carbon storage and total nitrogen storage.Available Phosphorus,C/N ratio,and Moisture Content are the main factors promoting soil organic carbon and total nitrogen accumulation.
文摘The Cenozoic strata are well developed in the northwest of Yunnan Province, where the eastern boundary of Qing—Zang (Qinghai—Xizang) plateau is located. The rich geo\|records in the Cenozoic strata can help us to recapitulate the evolution history of Qing—Zang plateau.1\ The Cenozoic Strata Ninglang Formation (Paleocene—Middle Eocene) is composed of massively bedded conglomerate , mudstone in the lower part, purple thinly bedded—medium bedded fine quartz sandstone and sandy shale in the upper part, 600m thick. Lijiang Formation (Upper Eocene) and Jinsichang Formation (Oligocene): conglomerate, with a little sandstone in lower part, claystone, with a little conglomerate in the upper part. Lijiang Formation unconformably overlies on Ninglang Formation or even older strata, 1500～2000m thick. Shuanghe Formation (Miocene): thinly—massively bedded muddy siltstone, fine sandstone, marl, with several layers of coal. It unconformably overlies on Jinsichang Formation or even older strata, 108m thick. Sanying Formation (Pliocene): Claystone, siltstone, with a little lignite in the middle and upper part, conglomerate at the base, 110m thick, widely spread in the northwest of Yunnan.Sheshan Formation (early Pleistocene): pebbles, sands and clay layers. It unconformably overlies on the older strata, 100～187m thick.Heyunsi Formation (middle Pleistocene): poorly sorted and poorly rounded gravel and sands, 100～347m thick.Upper Pleistocene Series: glaciers—gravel, sands and clays; alluvial—sandy gravel layer(terraces); lacustrine—fine sand, silt and clay layer, 100 m thick.Holocene Series: lacustrine—sand, silt and clay layers; alluvial—sandy gravel layer (terraces), 50m thick.
文摘The southeast margin of Tibet plateau mainly consists of the Western Yunnan plateau (WYP). The uplift and denudation at the southeast margin of Tibet plateau can be represented by that of the WYP. Based on the uplift of ancient plantain surface, river terrace and sedimentary response in peripheral basins of the WYP, suggest that the WYP experienced a rapid uplift and denudation in Quaternary. The WYP have been uplifted about 610～700m, and eroded away about 1095～1600m since Quaternary, average denudation rate reach 0 68～0 94mm/a. Uplift rates in different time interval were calculated according to river terrace. Relations between WYP and Tibetan plateau are discussed further..The Yinggehai basin located at the south termination of the Red River fault, it is the younger (mainly Neogene) pull\|apart basin, which developed at releasing bend of the Red River right\|lateral wrench fault. Since the Neogene, the subsidence center of the Yinggehai basin shifted southward and, connected with the Southeast Hainan basin. Both basins collected large amounts of the Holocene and Quaternary deposits of marine origin. They are peripheral marine basin of the WYP.. Silicate clastic sediments in both basins have been large supported from the WYP into both basins through the Red River system. The total volumes derived from the WYP in the Neogene and Quaternary is 2 8004×10 14 t(1 and 5 1206×10 14 t. The sedimentation rate in Yinggehai basin rose from 0 52mm/a in the Neogene to 1 39mm/a in the Quaternary. The facts that accumulation volume and sedimentation rate rose greatly after the Neogene, suggested a rapid uplift in the WYP. The rapid uplift was responsible for the unconformity between the Neogene and Quaternary. Elevation of ancient planation surface,and river terrace supported the rapid uplift of the WYP also. The ancient planation surface was elevated from 2500～2600m to 3000～3200m during Quaternary, seven terraces in Tue can be traced through the field area in elevation from 20 5m to 612m above the modern river surface in the Lancang River. The Jinsha River also incised into bed rocks about 700m in Shigu. All the facts suggest that southeast margin of Tibet plateau rose rapidly; the plateau was elevated about 610～700m in the Quaternary.
文摘In south\|eastern margin of Tibetan plateau, the Western Yunnan area of China, the NNW\|striking faults are dominant active structures. Their dextral strike\|slips cause conjugate slips along NE\|striking faults, and these left shears induce blocks’ clockwise rotations along vertical axes. For example, Simao Block in the south part of Western Yunnan is bounded by Red River Fault (east), Lancang—Gengma Fault (west), Nandinghe Fault (north), and Dian Bien Phu Fault (south); and the right shears of Red River Fault and Lancang—Gengma Fault induced conjugate left shear along Nandinghe Fault and Dian Bien Phu Fault, and laters’ sinistral slips caused clockwise rotation of the Block. This rotation has been proved by geodetic measurements (Jiang, et al., 1993) and palaeomagnetic measurement (Wu, et al., 1987). In Pu’er area, which is located in the central part of Simao Block, several small\|scale blocks are clockwise rotated by sinistral shears of NE\|striking faults (Wang Yang, 1996). Block rotation along vertical axis is main active deformation style in Western Yunnan.
