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您的检索式：作者名="MA ChuanLian"
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| 1 | Long-term cycles in the carbon reservoir of the Quaternary ocean: a perspective from the South China Sea显示文摘In recent years,long-term,high-resolution records from the deep sea and ice-cores have ofered new research opportunities for Quaternary science.Paleoclimate studies are no longer restricted to individual glacial cycles,but extend to long-term(≥105 yr)processes across those cycles.Ocean Drilling Program Leg 184 of the South China Sea in 1999 uncovered well-preserved sediment sections,in which three long-term cycles in Pleistocene carbon isotope(δ13C)sequence have been found and demonstrated to be common in the global ocean.Subsequent discoveries conirm the existence of long-term processes of 105yr in both the hydrologic(ice-sheet changes)and carbon(biogeochemical changes)cycles,posing the question whether the two processes are related.he present review shows that the long-eccentricity cycles prevail throughout theδ13C and other biogeochemical records in geologic history,and 400-kyr cycles in the oceanicδ13C sequence before the Quaternary can be hypothetically explained by changes in ratio between particulate and dissolved organic carbon(POC/DOC)in the ocean,depending on the monsoon-controlled nutrient supply.his is a‘DOC hypothesis’.However,ocean restructuring at 1.6 Ma marked by the isolation of a sluggish abyss under the Southern Ocean has obscured the long-eccentricity 400-kyr signal in oceanicδ13C.he last million-year period has experienced two major changes in the climate regime,namely the mid-Pleistocene transition(MPT)centered at 0.9 Ma and the mid-Brunhes event(MBE)around 0.4 Ma.he MPT and MBE were preluded byδ13C maxima-III(δ13Cmax-III)~1.0 Ma andδ13Cmax-II~0.5 Ma,respectively.Together with similar hydroclimatic phenomena over corresponding glacial cycles,the two groups of hydrologic and biogeochemical events appear to have been driven largely by oceanographic changes in the Southern Ocean.herefore,we interpret that the long-term biogeochemical processes originating from the Southern Ocean must have played a crucial role in Quaternary ice-sheet waxing and waning. | PinXian Wang QianYu Li Jun Tian ZhiMin Jian ChuanLian Liu Li Li WenTao Ma | 2014 | National Science Review2014，1，1： | 23 |
| 2 | Horror Video Recognition Based on Fuzzy Comprehensive Evolution显示文摘 | SONG Wei YANG Pei YANG Guosheng MA ChuanLian YU Jing LIMing | 2014 | China Communications2014，11，A02： | 2 |
| 3 | Calcareous nannofossil changes in the Early Oligocene linked to nutrient and atmospheric CO2显示文摘Rapid changes on nutrient supply and CO2 concentration that occurred in the northern South China Sea(SCS)during the Early Oligocene,provides an ideal natural laboratory,allowing us to peer into the coccolithophores’physiology in the geological records.In this study,we established a new nannofossil assemblage index,termed as E^*ratio,which is calculated by the relative abundance of eutrophic taxa and meso-oligotrophic taxa(E^*=e/e+c,where e is eutrophic taxa,and c is meso-oligotrophic taxa)Eutrophic taxa include small Reticulofenestra,Reticulofenestra lockeri group,Reticulofenestra bisecta group and Coccolithus pelagicus group,while meso-oligotrophic taxa include Cyclicargolithus spp.The E^*ratio is well correlated with nutrient proxy during the Early Oligocene,while with different covarying patterns under the higher and lower CO2 condition.By comparing the assemblage changes to the published data,we suggest that coccolithophores may change the way they use carbon source and nutrient with the decline of CO2.Furthermore,this implies a possible initiation of the carbon concentrating mechanism. | Ruigang Ma Haizhang Yang Xiaobo Jin Zhao Zhao Gongcheng Zhang Chuanlian Liu | 2020 | Acta Oceanologica Sinica2020，39，10： | 0 |
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