From 1985 to 1987, four new localities with abundant fossil mammals were dis-covered by Cao, Tian and others in the Zhoukoudian (Choukoutien) area, Beijing. They are theEast, West, Shangdian and Donglingzi caves. The ...From 1985 to 1987, four new localities with abundant fossil mammals were dis-covered by Cao, Tian and others in the Zhoukoudian (Choukoutien) area, Beijing. They are theEast, West, Shangdian and Donglingzi caves. The East Cave fauna consists of 28 speices ofmammals and its age is middle Early Pleistocene. The East Cave assemblage shows that a tem-perature-falling event took place at around 1.20 Ma B.P. at Zhoukoudian. Sixteen species ofmammals were collected from the West Cave, which are mainly forms of late Early Pleistoceneage. The West Cave fauna represents a transitional fauna from the East Cave fauna (dry-cold)to the fauna (warm) at locality 9. The Shangdian Cave fauna is composed of four forms, beingMiddle Pleistocene in age. The Donglingzi Cave fauna contains 21 Late Pleistocene forms. Inthe cave two fossil horizons may be distinguished. The age of the lower horizon is early LatePleistocene, which is equivalent to that of the New Cave fauna; while the fauna of the upper ho-rizon may be correlated with the Upper Cave fauna.展开更多
The response of grain quality traits to cold-water irrigation and its correlation with cold tolerance were studied in 11 japonica rice varieties from Yunnan Province, China. The results indicated that the response of ...The response of grain quality traits to cold-water irrigation and its correlation with cold tolerance were studied in 11 japonica rice varieties from Yunnan Province, China. The results indicated that the response of grain quality traits to the cold-water stress varied with rice varieties and grain quality traits. Under the cold-water stress, grain width, chalky rice rate, whiteness, 1000-grain weight, brown rice rate, taste meter value, peak viscosity, trough viscosity, breakdown viscosity and final viscosity significantly decreased, whereas grain length-width ratio, head rice rate, alkali digestion value, protein content and setback viscosity markedly increased. However, the other traits such as grain length, amylose content, milled rice rate, peak viscosity time and pasting temperature were not significantly affected by the cold-water stress. Significant correlations were discovered between phenotypic acceptability and cold response indices of taste meter value, protein content, peak viscosity and breakdown viscosity. Therefore, it would be very important to improve the cold tolerance of Yunnan rice varieties in order to stabilize and improve their eating quality.展开更多
Wave-current interaction and its effects on the hydrodynamic environment in the Beibu Gulf(BG) have been investigated via employing the Coupled Ocean–Atmosphere–Wave–Sediment Transport(COAWST) modeling system. The ...Wave-current interaction and its effects on the hydrodynamic environment in the Beibu Gulf(BG) have been investigated via employing the Coupled Ocean–Atmosphere–Wave–Sediment Transport(COAWST) modeling system. The model could simulate reasonable hydrodynamics in the BG when validated by various observations.Vigorous tidal currents refract the waves efficiently and make the seas off the west coast of Hainan Island be the hot spot where currents modulate the significant wave height dramatically. During summer, wave-enhanced bottom stress could weaken the near-shore component of the gulf-scale cyclonic-circulation in the BG remarkably, inducing two major corresponding adjustments: Model results reveal that the deep-layer cold water from the southern BG makes critical contribution to maintaining the cold-water mass in the northern BG Basin.However, the weakened background circulation leads to less cold water transported from the southern gulf to the northern gulf, which finally triggers a 0.2℃ warming in the cold-water mass area;In the top areas of the BG, the suppressed background circulation reduces the transport of the diluted water to the central gulf. Therefore, more freshwater could be trapped locally, which then triggers lower sea surface salinity(SSS) in the near-field and higher SSS in the far-field.展开更多
About 70 examples of Quaternary fauna in China's tropics are enumerated in this paper. Of which about 40% of the examples can be found even in cooling stages, showing the smaller amplitude of climatic fluctuation ...About 70 examples of Quaternary fauna in China's tropics are enumerated in this paper. Of which about 40% of the examples can be found even in cooling stages, showing the smaller amplitude of climatic fluctuation during Quaternary. According to the temporal and spatial distribution of tropical faunas, the following characters of climate variation can be evidenced: two main cycles in Early Pleistocene, three main cycles in Middle Pleistocene, two main cycles in Late Pleistocene and Holocene Megathermal. The drop in temperature during the Latest Glacial Period and Neoglaciation has not endangered the existence of tropical faunas. With influence of cooling fluctuation during historical period, some faunas have removed southwards progressively, but disappearance of these animals in China's tropics was mainly the result of artificial factors.展开更多
There are 3048 species of fish occurring in the China Seas (CS), of which at least 2321 species are found in the South China Sea (SCS), belonging to 35 orders, 236 families and 822 genera. The fish species diversi...There are 3048 species of fish occurring in the China Seas (CS), of which at least 2321 species are found in the South China Sea (SCS), belonging to 35 orders, 236 families and 822 genera. The fish species diversity is analyzed in this paper based on biogeography, biostatistics, fishing methods, etc. It is found that the regional environment, especially biological factors, plays an important role in the distribution of faunas, and there are two fish faunas in the SCS, one in the north and another in the center and south. This regional division is of value for sustainable fishery production and eiTlcient management of fishery resources.展开更多
Using the UVic Earth System Model, this study simulated the change of seawater chemistry and analyzed the chemical habitat surrounding shallow- and cold-water coral reefs from the year 1800 to 2300 employing RCP2.6, R...Using the UVic Earth System Model, this study simulated the change of seawater chemistry and analyzed the chemical habitat surrounding shallow- and cold-water coral reefs from the year 1800 to 2300 employing RCP2.6, RCP4.5, RCP6.0, and RCP8.5 scenarios. The model results showed that the global ocean will continue to absorb atmospheric CO2. Global mean surface ocean temperature will rise 1.1-2.8 K at the end of the 21st century across RCP scenarios. Meanwhile, the global mean surface ocean pH will drop 0.14--0.42 and the ocean surface mean con- centration of carbonate will decrease 20%--51% across the RCP scenarios. The saturated state of sea water with respect to calcite carbonate minerals (t2) will decrease rapidly. During the pre-industrial period, 99% of the shallow-water coral reefs were surrounded by seawater with t2 〉 3.5 and 87% of the deep-sea coral reefs were surrounded by seawater with aragonite supersaturation. Within the 21st century, except for the high mitigation scenario of RCP2.6, almost none shallow-water coral reefs will be surrounded by seawater with g2 〉 3.5. Under the intensive emission scenario of RCP8.5, by the year 2100, the aragonite saturation horizon will rise to 308 m under the sea surface from 1138 m at the pre- industrial period, thus 73% of the cold-water coral reefs will be surrounded by seawater with aragonite undersaturation. By the year 2300, only 5% of the cold-water coral reefs will be surrounded by seawater with aragonite supersaturation.展开更多
This review aims to fill the voids and to update the checklist of sandfly fauna along with its spatial distribution in India.Resource databases i.e.either online or offline were searched to deduce the information to s...This review aims to fill the voids and to update the checklist of sandfly fauna along with its spatial distribution in India.Resource databases i.e.either online or offline were searched to deduce the information to systematize the Indian sandfly fauna.Articles/data retrieved were screened and analysed to further update the available latest checklist.The species name and authorship were given in accord with the International Code for Zoological Nomenclature.We compiled an updated checklist of reported Indian sandfly species along with their state-wise distribution till 2022 as per published literature.Kerala has maximum number of species reports when compared to other endemic states and states with pockets of transmission.Phlebotomus argentipes is the most widely distributed,recorded so far,followed by other Sergentomiya and Phlebotomus species in India.In this review,we have also described the vector and non-vector species of sandfly prevalent in different parts of the country.Phlebotoiella eoindianensis,an amber fossil sandfly species recorded from Gujarat might be older than other records of Indian sandfly fauna.So far 69 species(4 genera and 15 subgenera/groups)of Phlebotomine sandflies have been recorded in India.Proper knowledge of species diversity and its distribution is a prerequisite for planning a systematic vector control strategy and disease management.展开更多
Objective The Devonian bivalves are well developed, highly diversified and widely distributed in Guangxi. However, they have not been well studied previously, although several papers have dealt with it. Meanwhile, the...Objective The Devonian bivalves are well developed, highly diversified and widely distributed in Guangxi. However, they have not been well studied previously, although several papers have dealt with it. Meanwhile, the biodiversity change of bivalves which is one of the most important benthos during Devonian in South China has not been studied yet. The aim of present project is focused on the study of systematic palaeontology, the life-habits, of Devonian bivalves of Guangxi.展开更多
Soil faunas account for 23%of known animal species and play a crucial role in ecosystem processes such as mineralizing nutrients,regulating microbial community composition,forming soil aggregates,and enhancing primary...Soil faunas account for 23%of known animal species and play a crucial role in ecosystem processes such as mineralizing nutrients,regulating microbial community composition,forming soil aggregates,and enhancing primary productivity.However,due to global climate change,population density,community composition,and distribution patterns of soil fauna vary.Understanding the responses of soil fauna to major environmental change facilitate the conservation of biodiversity.Therefore,a review work of recent researches for analysing the effects of key environmental factors on soil fauna,such as warming,drought,food quality,and soil physical-chemical properties was studied.For most species,warming may exert a positive effect on their abundance and population development,however,it can inhibit the survival and reproduction of hibernating species.Drought leads to low soil porosity and water holding capacity,which reduces soil fauna population and changes their community composition.Drought also can reduce the coverage of flora and alter microclimate of the soil surface,which in turn indirectly reduces fauna abundance.Climate warming and elevated atmospheric carbon dioxide can reduce litter quality,which will force soil fauna to change their dietary choices(from higher-quality foods to poor quality foods)and reduce reproduction for survival.However,it is still predicted that enhanced species richness of plant(or litter)mixtures will positively affect soil fauna diversity.Habitat loss caused by the deterioration of soil physical-chemical property is primary factor affecting soil fauna.We mainly discuss the threats of increased salinity(a major factor in arid land)to soil fauna and their potential responses to anthropogenic disturbance in saline soils.The increase in soil salinity can override other factors that favour habitat specialists,leading to negative effects on soil fauna.Moreover,we find that more studies are needed to explore the responses of soil fauna in saline soils to human activities.And the relationship of important ecological processes with soil fauna density,community structure,and diversity needs to be redefined.展开更多
基金This study was a contribution to the 30th IGC Project 96-30-16 supported by the State Planning Commission and the Beijing Bureau of Geology and Mineral Resources.Yuan Lingsheng,Li Chang'an,Li Longyin,Chen Lianfang,Chi Zhenqing and Zhang Xujiao also took
文摘From 1985 to 1987, four new localities with abundant fossil mammals were dis-covered by Cao, Tian and others in the Zhoukoudian (Choukoutien) area, Beijing. They are theEast, West, Shangdian and Donglingzi caves. The East Cave fauna consists of 28 speices ofmammals and its age is middle Early Pleistocene. The East Cave assemblage shows that a tem-perature-falling event took place at around 1.20 Ma B.P. at Zhoukoudian. Sixteen species ofmammals were collected from the West Cave, which are mainly forms of late Early Pleistoceneage. The West Cave fauna represents a transitional fauna from the East Cave fauna (dry-cold)to the fauna (warm) at locality 9. The Shangdian Cave fauna is composed of four forms, beingMiddle Pleistocene in age. The Donglingzi Cave fauna contains 21 Late Pleistocene forms. Inthe cave two fossil horizons may be distinguished. The age of the lower horizon is early LatePleistocene, which is equivalent to that of the New Cave fauna; while the fauna of the upper ho-rizon may be correlated with the Upper Cave fauna.
基金funded by the project 2006 NG 04 of Yunnan Province,Chinathe International corporation project between the Yunnan Academy of Agricultural Sciences of China and the National Institute of Crop Science,Rural Development Administration of Korea
文摘The response of grain quality traits to cold-water irrigation and its correlation with cold tolerance were studied in 11 japonica rice varieties from Yunnan Province, China. The results indicated that the response of grain quality traits to the cold-water stress varied with rice varieties and grain quality traits. Under the cold-water stress, grain width, chalky rice rate, whiteness, 1000-grain weight, brown rice rate, taste meter value, peak viscosity, trough viscosity, breakdown viscosity and final viscosity significantly decreased, whereas grain length-width ratio, head rice rate, alkali digestion value, protein content and setback viscosity markedly increased. However, the other traits such as grain length, amylose content, milled rice rate, peak viscosity time and pasting temperature were not significantly affected by the cold-water stress. Significant correlations were discovered between phenotypic acceptability and cold response indices of taste meter value, protein content, peak viscosity and breakdown viscosity. Therefore, it would be very important to improve the cold tolerance of Yunnan rice varieties in order to stabilize and improve their eating quality.
基金The Program for Scientific Research Start-up Funds of Guangdong Ocean University under contract No.101302/R18001the Fund of Southern Marine Science and Engineering Guangdong Laboratory(Zhanjiang)under contract No.ZJW-2019-08+1 种基金the National Key Research and Development Program of China under contract No.2016YFC1401403the National Natural Science Foundation of China under contract Nos 41476009 and 41776034
文摘Wave-current interaction and its effects on the hydrodynamic environment in the Beibu Gulf(BG) have been investigated via employing the Coupled Ocean–Atmosphere–Wave–Sediment Transport(COAWST) modeling system. The model could simulate reasonable hydrodynamics in the BG when validated by various observations.Vigorous tidal currents refract the waves efficiently and make the seas off the west coast of Hainan Island be the hot spot where currents modulate the significant wave height dramatically. During summer, wave-enhanced bottom stress could weaken the near-shore component of the gulf-scale cyclonic-circulation in the BG remarkably, inducing two major corresponding adjustments: Model results reveal that the deep-layer cold water from the southern BG makes critical contribution to maintaining the cold-water mass in the northern BG Basin.However, the weakened background circulation leads to less cold water transported from the southern gulf to the northern gulf, which finally triggers a 0.2℃ warming in the cold-water mass area;In the top areas of the BG, the suppressed background circulation reduces the transport of the diluted water to the central gulf. Therefore, more freshwater could be trapped locally, which then triggers lower sea surface salinity(SSS) in the near-field and higher SSS in the far-field.
基金National Natural Science Foundation of China,No.40071011No.49271070
文摘About 70 examples of Quaternary fauna in China's tropics are enumerated in this paper. Of which about 40% of the examples can be found even in cooling stages, showing the smaller amplitude of climatic fluctuation during Quaternary. According to the temporal and spatial distribution of tropical faunas, the following characters of climate variation can be evidenced: two main cycles in Early Pleistocene, three main cycles in Middle Pleistocene, two main cycles in Late Pleistocene and Holocene Megathermal. The drop in temperature during the Latest Glacial Period and Neoglaciation has not endangered the existence of tropical faunas. With influence of cooling fluctuation during historical period, some faunas have removed southwards progressively, but disappearance of these animals in China's tropics was mainly the result of artificial factors.
基金supported financially by projects of the National Science Foundation of China and School of Economics of Shandong Province.
文摘There are 3048 species of fish occurring in the China Seas (CS), of which at least 2321 species are found in the South China Sea (SCS), belonging to 35 orders, 236 families and 822 genera. The fish species diversity is analyzed in this paper based on biogeography, biostatistics, fishing methods, etc. It is found that the regional environment, especially biological factors, plays an important role in the distribution of faunas, and there are two fish faunas in the SCS, one in the north and another in the center and south. This regional division is of value for sustainable fishery production and eiTlcient management of fishery resources.
基金supported by National Natural Science Foundation of China(41276073,41422503)National Key Basic Research Program of China(2015CB953601)+1 种基金Zhejiang University K.P.Chao's High Technology Development Foundationthe Fundamental Research Funds for the Central Universities
文摘Using the UVic Earth System Model, this study simulated the change of seawater chemistry and analyzed the chemical habitat surrounding shallow- and cold-water coral reefs from the year 1800 to 2300 employing RCP2.6, RCP4.5, RCP6.0, and RCP8.5 scenarios. The model results showed that the global ocean will continue to absorb atmospheric CO2. Global mean surface ocean temperature will rise 1.1-2.8 K at the end of the 21st century across RCP scenarios. Meanwhile, the global mean surface ocean pH will drop 0.14--0.42 and the ocean surface mean con- centration of carbonate will decrease 20%--51% across the RCP scenarios. The saturated state of sea water with respect to calcite carbonate minerals (t2) will decrease rapidly. During the pre-industrial period, 99% of the shallow-water coral reefs were surrounded by seawater with t2 〉 3.5 and 87% of the deep-sea coral reefs were surrounded by seawater with aragonite supersaturation. Within the 21st century, except for the high mitigation scenario of RCP2.6, almost none shallow-water coral reefs will be surrounded by seawater with g2 〉 3.5. Under the intensive emission scenario of RCP8.5, by the year 2100, the aragonite saturation horizon will rise to 308 m under the sea surface from 1138 m at the pre- industrial period, thus 73% of the cold-water coral reefs will be surrounded by seawater with aragonite undersaturation. By the year 2300, only 5% of the cold-water coral reefs will be surrounded by seawater with aragonite supersaturation.
基金supported by the Indian Council of Medical Research,New Delhi[Grant No.6/9-7(331)/2020/ECD-II].
文摘This review aims to fill the voids and to update the checklist of sandfly fauna along with its spatial distribution in India.Resource databases i.e.either online or offline were searched to deduce the information to systematize the Indian sandfly fauna.Articles/data retrieved were screened and analysed to further update the available latest checklist.The species name and authorship were given in accord with the International Code for Zoological Nomenclature.We compiled an updated checklist of reported Indian sandfly species along with their state-wise distribution till 2022 as per published literature.Kerala has maximum number of species reports when compared to other endemic states and states with pockets of transmission.Phlebotomus argentipes is the most widely distributed,recorded so far,followed by other Sergentomiya and Phlebotomus species in India.In this review,we have also described the vector and non-vector species of sandfly prevalent in different parts of the country.Phlebotoiella eoindianensis,an amber fossil sandfly species recorded from Gujarat might be older than other records of Indian sandfly fauna.So far 69 species(4 genera and 15 subgenera/groups)of Phlebotomine sandflies have been recorded in India.Proper knowledge of species diversity and its distribution is a prerequisite for planning a systematic vector control strategy and disease management.
基金financially supported by the National Natural Science Foundation of China No.41172025
文摘Objective The Devonian bivalves are well developed, highly diversified and widely distributed in Guangxi. However, they have not been well studied previously, although several papers have dealt with it. Meanwhile, the biodiversity change of bivalves which is one of the most important benthos during Devonian in South China has not been studied yet. The aim of present project is focused on the study of systematic palaeontology, the life-habits, of Devonian bivalves of Guangxi.
基金supported by the National Natural Science Foundation of China (31971448, U1803233)the Foundation of Science & Technology Department of Xinjiang Uygur Autonomous Region, China (2019XS28)the Youth Innovation Promotion Association of Chinese Academy of Sciences (2020433)
文摘Soil faunas account for 23%of known animal species and play a crucial role in ecosystem processes such as mineralizing nutrients,regulating microbial community composition,forming soil aggregates,and enhancing primary productivity.However,due to global climate change,population density,community composition,and distribution patterns of soil fauna vary.Understanding the responses of soil fauna to major environmental change facilitate the conservation of biodiversity.Therefore,a review work of recent researches for analysing the effects of key environmental factors on soil fauna,such as warming,drought,food quality,and soil physical-chemical properties was studied.For most species,warming may exert a positive effect on their abundance and population development,however,it can inhibit the survival and reproduction of hibernating species.Drought leads to low soil porosity and water holding capacity,which reduces soil fauna population and changes their community composition.Drought also can reduce the coverage of flora and alter microclimate of the soil surface,which in turn indirectly reduces fauna abundance.Climate warming and elevated atmospheric carbon dioxide can reduce litter quality,which will force soil fauna to change their dietary choices(from higher-quality foods to poor quality foods)and reduce reproduction for survival.However,it is still predicted that enhanced species richness of plant(or litter)mixtures will positively affect soil fauna diversity.Habitat loss caused by the deterioration of soil physical-chemical property is primary factor affecting soil fauna.We mainly discuss the threats of increased salinity(a major factor in arid land)to soil fauna and their potential responses to anthropogenic disturbance in saline soils.The increase in soil salinity can override other factors that favour habitat specialists,leading to negative effects on soil fauna.Moreover,we find that more studies are needed to explore the responses of soil fauna in saline soils to human activities.And the relationship of important ecological processes with soil fauna density,community structure,and diversity needs to be redefined.