The Meso-neoproterozoic Bayan Obo rift is located along the northern margin of the North China Craton,and was associated with the break-up of the Columbia supercontinent.During rift evolution,syn-sedimentary deformati...The Meso-neoproterozoic Bayan Obo rift is located along the northern margin of the North China Craton,and was associated with the break-up of the Columbia supercontinent.During rift evolution,syn-sedimentary deformation occurred due to tectonic activity and earthquakes.Seismic events are recorded in the Jianshan Formation of the Bayan Obo Group,Inner Mongolia,as soft sediment deformation structures in the central Bayan Obo rift.Druse calcite crystals and collapse breccias in the Jianshan Formation may provide information on the rift evolution.The druse calcite crystals are idiomorphic-columnar in shape and associated with graphite,pyrite,and quartz.δ^(13)C values of the graphite are−20‰,indicative of biogenic deoxygenation and formation in water.The druse calcite crystals are inorganic in origin and formed in water at a temperature of 55℃,based on calciteδ^(13)C andδ^(18)O data.The calcite grew in paleo-caves containing fault breccias,with heat derived from faulting.As such,the druse calcite crystals are important evidence for seismic events.The collapse breccias(i.e.,fault breccias)and other indicators of slip show that displacement occurred from NE to SW,which is different from the paleocurrent direction in the Jianshan Formation.The thickness of the collapse breccia is∼200 m,which represents the height of the fault scarp.The strike of the fault scarp was NE-SW,based on the distribution of the collapse breccia.The Bayan Obo and Yanliao rifts experienced rapid NW-SE extension,and developed similar deformation structures at ca.1.6 Ga related to break-up of the Columbia supercontinent.展开更多
<strong>Background:</strong> Druses of the papilla constitute abnormal deposits of calcified hyaline material at the level of the head of the optic nerve. They can be superficial or deep. <strong>Aim...<strong>Background:</strong> Druses of the papilla constitute abnormal deposits of calcified hyaline material at the level of the head of the optic nerve. They can be superficial or deep. <strong>Aim:</strong> The aim of this study is to show the utility of ocular ultrasound in ophthalmology in underdeveloped countries for the characterization of optic disc druse. <strong>Case Presentation:</strong> Our study relates to a clinical observation of buried papillary druses diagnosed by ocular ultrasound. The ophthalmologic examination revealed an aspect of false papillary edema in the fundus. The ocular ultrasound revealed hyperechogenic deposits buried in the papillary margins, which suggests the deep papillary druses. <strong>Conclusion:</strong> Ocular ultrasound still has a prominent place in the diagnosis of certain eye conditions despite the new sophisticated means available to ophthalmology to date.展开更多
Leaves of twenty-two (22) species of Combretum in Nigeria were examined for occurrence and distribution of different types and sizes of ergastic substances (calcium oxalate crystals). Fresh and herbarium specimens wer...Leaves of twenty-two (22) species of Combretum in Nigeria were examined for occurrence and distribution of different types and sizes of ergastic substances (calcium oxalate crystals). Fresh and herbarium specimens were used for the study. These specimens were wax embedded, sectioned, mounted and micro-photographed using Leica WILD MPS 52 microscope camera on Leitz Diaplan microscope. Results revealed two types of calcium oxalate crystals—crystal sand and druses. Based on the observed differences in the size of the crystals, three groups of calcium oxalate crystals are reported [large crystals: 180.0 - 360.0 μm (241 ± 44.57 μm), moderate crystals: 90.0 - 144.0 μm (117.0 ± 20.60 μm), and small crystals: 18.0 - 72.0 μm (50.21 ± 20.42 μm)]. Crystal sand was found only in Combretum sp. 1 but druses of varying sizes predominated amongst species of the genus. Crystals were distributed within the spongy mesophyll, palisade mesophyll, sub-epidermis adaxial, sub-epidermis abaxial and between the palisade and spongy mesophyll. The findings of this work provide information on the occurrence and distribution of the crystals in the leaf epidermis of these taxa in Nigeria. The formation, occurrence and distribution of the crystal type in the Combretum species constitute dependable taxonomic character especially when combined with other characters.展开更多
Multipurpose cactus pear plant with great potential as a source of food and livestock faced a threat from Dactylopius spp in different countries. Specifically, D. coccus is an important pest damaging significant areas...Multipurpose cactus pear plant with great potential as a source of food and livestock faced a threat from Dactylopius spp in different countries. Specifically, D. coccus is an important pest damaging significant areas in Tigray-Ethiopia. Using pest-resistant cultivars is an important element of an integrated pest management strategy, and studying the mechanisms of resistance is vital. It can be chemical or physical such as oxalate crystals and other cladode characteristics. Cladode features of six cultivars (three O. ficus-indica, two O. cochenillifera, and one O. robusta) were examined for resistance to D. coccus in a completely randomized design (CRD) with three replications. ‘Rojo Pelón’ (O. ficus-indica), ‘Robusta’ (O. robusta), and ‘Bioplástico’ (O. cochenillifera) are resistant cultivars;and ‘Atlixco’ and ‘Chicomostoc’ (O. ficus-indica) and ‘Nopalea’ (O. cochenillifera) are susceptible. Cultivars showed a significant difference in cladode weight in g, and cladode length, cladode width, and cladode thickness in cm, where cladode thickness was higher in ‘Rojo Pelón’ followed by ‘Robusta’. Calcium oxalates number per mm was higher in ‘Bioplástico’ (20.7 ± 2.08) followed by ‘Robusta’ (18.9 ± 2.31) and ‘Rojo Pelón’ (15.9 ± 0.34);and similarly, epidermis thickness found higher in ‘Bioplástico’ (0.21 ± 0.032) and ‘Robusta’ (0.19 ± 0.014), but similar with ‘Rojo Pelón’ (0.18 ± 0.026). However, cuticle thickness didn’t show a difference among cultivars. Cladode thickness, calcium oxalate number, and epidermis thickness had positive correlations with resistance. These results demonstrate that calcium oxalate number and epidermis thickness might have a positive role in D. coccus resistance in O. ficus-indica. This feeding-barring role and the insect-plant interaction need to be studied.展开更多
基金supported by the National Natural Science Foundation of China(Nos.41772227,41872232)supported by the Inner Mongolia Mapping Programs(Nos.1212010811001,1212011120700,DD20160045,1212010510506)awarded to Zhiguang Zhou and administered by the Institute of Geological Survey,China University of Geosciences(Beijing).
文摘The Meso-neoproterozoic Bayan Obo rift is located along the northern margin of the North China Craton,and was associated with the break-up of the Columbia supercontinent.During rift evolution,syn-sedimentary deformation occurred due to tectonic activity and earthquakes.Seismic events are recorded in the Jianshan Formation of the Bayan Obo Group,Inner Mongolia,as soft sediment deformation structures in the central Bayan Obo rift.Druse calcite crystals and collapse breccias in the Jianshan Formation may provide information on the rift evolution.The druse calcite crystals are idiomorphic-columnar in shape and associated with graphite,pyrite,and quartz.δ^(13)C values of the graphite are−20‰,indicative of biogenic deoxygenation and formation in water.The druse calcite crystals are inorganic in origin and formed in water at a temperature of 55℃,based on calciteδ^(13)C andδ^(18)O data.The calcite grew in paleo-caves containing fault breccias,with heat derived from faulting.As such,the druse calcite crystals are important evidence for seismic events.The collapse breccias(i.e.,fault breccias)and other indicators of slip show that displacement occurred from NE to SW,which is different from the paleocurrent direction in the Jianshan Formation.The thickness of the collapse breccia is∼200 m,which represents the height of the fault scarp.The strike of the fault scarp was NE-SW,based on the distribution of the collapse breccia.The Bayan Obo and Yanliao rifts experienced rapid NW-SE extension,and developed similar deformation structures at ca.1.6 Ga related to break-up of the Columbia supercontinent.
文摘<strong>Background:</strong> Druses of the papilla constitute abnormal deposits of calcified hyaline material at the level of the head of the optic nerve. They can be superficial or deep. <strong>Aim:</strong> The aim of this study is to show the utility of ocular ultrasound in ophthalmology in underdeveloped countries for the characterization of optic disc druse. <strong>Case Presentation:</strong> Our study relates to a clinical observation of buried papillary druses diagnosed by ocular ultrasound. The ophthalmologic examination revealed an aspect of false papillary edema in the fundus. The ocular ultrasound revealed hyperechogenic deposits buried in the papillary margins, which suggests the deep papillary druses. <strong>Conclusion:</strong> Ocular ultrasound still has a prominent place in the diagnosis of certain eye conditions despite the new sophisticated means available to ophthalmology to date.
文摘Leaves of twenty-two (22) species of Combretum in Nigeria were examined for occurrence and distribution of different types and sizes of ergastic substances (calcium oxalate crystals). Fresh and herbarium specimens were used for the study. These specimens were wax embedded, sectioned, mounted and micro-photographed using Leica WILD MPS 52 microscope camera on Leitz Diaplan microscope. Results revealed two types of calcium oxalate crystals—crystal sand and druses. Based on the observed differences in the size of the crystals, three groups of calcium oxalate crystals are reported [large crystals: 180.0 - 360.0 μm (241 ± 44.57 μm), moderate crystals: 90.0 - 144.0 μm (117.0 ± 20.60 μm), and small crystals: 18.0 - 72.0 μm (50.21 ± 20.42 μm)]. Crystal sand was found only in Combretum sp. 1 but druses of varying sizes predominated amongst species of the genus. Crystals were distributed within the spongy mesophyll, palisade mesophyll, sub-epidermis adaxial, sub-epidermis abaxial and between the palisade and spongy mesophyll. The findings of this work provide information on the occurrence and distribution of the crystals in the leaf epidermis of these taxa in Nigeria. The formation, occurrence and distribution of the crystal type in the Combretum species constitute dependable taxonomic character especially when combined with other characters.
文摘Multipurpose cactus pear plant with great potential as a source of food and livestock faced a threat from Dactylopius spp in different countries. Specifically, D. coccus is an important pest damaging significant areas in Tigray-Ethiopia. Using pest-resistant cultivars is an important element of an integrated pest management strategy, and studying the mechanisms of resistance is vital. It can be chemical or physical such as oxalate crystals and other cladode characteristics. Cladode features of six cultivars (three O. ficus-indica, two O. cochenillifera, and one O. robusta) were examined for resistance to D. coccus in a completely randomized design (CRD) with three replications. ‘Rojo Pelón’ (O. ficus-indica), ‘Robusta’ (O. robusta), and ‘Bioplástico’ (O. cochenillifera) are resistant cultivars;and ‘Atlixco’ and ‘Chicomostoc’ (O. ficus-indica) and ‘Nopalea’ (O. cochenillifera) are susceptible. Cultivars showed a significant difference in cladode weight in g, and cladode length, cladode width, and cladode thickness in cm, where cladode thickness was higher in ‘Rojo Pelón’ followed by ‘Robusta’. Calcium oxalates number per mm was higher in ‘Bioplástico’ (20.7 ± 2.08) followed by ‘Robusta’ (18.9 ± 2.31) and ‘Rojo Pelón’ (15.9 ± 0.34);and similarly, epidermis thickness found higher in ‘Bioplástico’ (0.21 ± 0.032) and ‘Robusta’ (0.19 ± 0.014), but similar with ‘Rojo Pelón’ (0.18 ± 0.026). However, cuticle thickness didn’t show a difference among cultivars. Cladode thickness, calcium oxalate number, and epidermis thickness had positive correlations with resistance. These results demonstrate that calcium oxalate number and epidermis thickness might have a positive role in D. coccus resistance in O. ficus-indica. This feeding-barring role and the insect-plant interaction need to be studied.
