Gao, Yongjun

[["dc.bibliographiccitation.firstpage","5072"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","5083"],["dc.bibliographiccitation.volume","24"],["dc.contributor.author","Wallach, Daniel"],["dc.contributor.author","Martre, Pierre"],["dc.contributor.author","Liu, Bing"],["dc.contributor.author","Asseng, Senthold"],["dc.contributor.author","Ewert, Frank"],["dc.contributor.author","Thorburn, Peter J."],["dc.contributor.author","van Ittersum, Martin"],["dc.contributor.author","Aggarwal, Pramod K."],["dc.contributor.author","Ahmed, Mukhtar"],["dc.contributor.author","Basso, Bruno"],["dc.contributor.author","Biernath, Christian"],["dc.contributor.author","Cammarano, Davide"],["dc.contributor.author","Challinor, Andrew J."],["dc.contributor.author","De Sanctis, Giacomo"],["dc.contributor.author","Dumont, Benjamin"],["dc.contributor.author","Eyshi Rezaei, Ehsan"],["dc.contributor.author","Fereres, Elias"],["dc.contributor.author","Fitzgerald, Glenn J."],["dc.contributor.author","Gao, Y."],["dc.contributor.author","Garcia-Vila, Margarita"],["dc.contributor.author","Gayler, Sebastian"],["dc.contributor.author","Girousse, Christine"],["dc.contributor.author","Hoogenboom, Gerrit"],["dc.contributor.author","Horan, Heidi"],["dc.contributor.author","Izaurralde, Roberto C."],["dc.contributor.author","Jones, Curtis D."],["dc.contributor.author","Kassie, Belay T."],["dc.contributor.author","Kersebaum, Kurt C."],["dc.contributor.author","Klein, Christian"],["dc.contributor.author","Koehler, Ann-Kristin"],["dc.contributor.author","Maiorano, Andrea"],["dc.contributor.author","Minoli, Sara"],["dc.contributor.author","Müller, Christoph"],["dc.contributor.author","Naresh Kumar, Soora"],["dc.contributor.author","Nendel, Claas"],["dc.contributor.author","O'Leary, Garry J."],["dc.contributor.author","Palosuo, Taru"],["dc.contributor.author","Priesack, Eckart"],["dc.contributor.author","Ripoche, Dominique"],["dc.contributor.author","Rötter, Reimund P."],["dc.contributor.author","Semenov, Mikhail A."],["dc.contributor.author","Stöckle, Claudio"],["dc.contributor.author","Stratonovitch, Pierre"],["dc.contributor.author","Streck, Thilo"],["dc.contributor.author","Supit, Iwan"],["dc.contributor.author","Tao, Fulu"],["dc.contributor.author","Wolf, Joost"],["dc.contributor.author","Zhang, Zhao"],["dc.date.accessioned","2020-12-10T18:28:42Z"],["dc.date.available","2020-12-10T18:28:42Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1111/gcb.14411"],["dc.identifier.issn","1354-1013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76386"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Multimodel ensembles improve predictions of crop-environment-management interactions"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","65"],["dc.bibliographiccitation.journal","The International Forestry Review"],["dc.bibliographiccitation.lastpage","84"],["dc.bibliographiccitation.volume","17"],["dc.contributor.author","Skutsch, Margaret"],["dc.contributor.author","Borrego, Armonia"],["dc.contributor.author","Morales-Barquero, Lucia"],["dc.contributor.author","Paneque-Galvez, J."],["dc.contributor.author","Salinas-Melgoza, M."],["dc.contributor.author","Ramirez, M. I."],["dc.contributor.author","Perez-Salicrup, D."],["dc.contributor.author","Benet, D."],["dc.contributor.author","Monroy, S."],["dc.contributor.author","Gao, Y."],["dc.date.accessioned","2018-11-07T10:00:17Z"],["dc.date.available","2018-11-07T10:00:17Z"],["dc.date.issued","2015"],["dc.description.abstract","In Mexico, REDD+ is being presented as a win-win policy enabling forest communities to benefit financially and diversify their income sources while preserving and increasing their forest carbon stocks through more sustainable management. Under the national programme, it is expected that forest communities will have opportunities to tailor their own approaches. However, to date there is little understanding about what opportunities and constraints exist in reality for forest communities to contribute to REDD+, and even less about how their members perceive these opportunities. We assess potential and constraints at community level and investigate perceptions about opportunities in REDD+ and strategies that communities are currently envisaging for participation, in seven communities in the Ayuquila River Basin and around the Chamela-Cuixmala Biosphere Reserve in Jalisco, and in the area surrounding the Monarch Butterfly Reserve in Michoacan. We find that there is more opportunity for reduced degradation and forest enhancement than for reduced deforestation, in all the communities; that it may be difficult to establish additionality for REDD+ activities in some communities; that the amount of forest resource per community may greatly affect the potential to participate; that the presence of people with no land rights may complicate the distribution of benefits; that communities expect REDD+ in general to follow the Payment for Environmental Services model, and that lack of information about what activities may count as REDD+ activities and what level of financial rewards may be expected mean that communities cannot at present adequately appraise whether REDD+ will be worth their while or not."],["dc.identifier.isi","000351672700005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37770"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Commonwealth Forestry Assoc"],["dc.relation.issn","2053-7778"],["dc.relation.issn","1465-5489"],["dc.title","Opportunities, constraints and perceptions of rural communities regarding their potential to contribute to forest landscape transitions under REDD plus : case studies from Mexico"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","857"],["dc.bibliographiccitation.issue","5-6"],["dc.bibliographiccitation.journal","American Mineralogist"],["dc.bibliographiccitation.lastpage","863"],["dc.bibliographiccitation.volume","90"],["dc.contributor.author","Zhang, Z. M."],["dc.contributor.author","Rumble, D."],["dc.contributor.author","Liou, J. G."],["dc.contributor.author","Xiao, Y. L."],["dc.contributor.author","Gao, Y. J."],["dc.date.accessioned","2018-11-07T11:01:38Z"],["dc.date.available","2018-11-07T11:01:38Z"],["dc.date.issued","2005"],["dc.description.abstract","The Qinglongshan O- and H-isotope anomaly occurs within a coesite-bearing, eclogite-facies regional metamorphic belt in Eastern China near Donghai in Jiangsu province. The anomaly is defined by low values of delta(18)O and delta D. Garnets from eclogite have delta(18)O as low as -11 parts per thousand and rutiles are -15 parts per thousand (VSMOW). Phengites have delta D of -120 parts per thousand (VSMOW). The anomaly is Neoproterozoic in age. Surface outcrops of coesite-eclogite-facies rocks with unusually low delta(18)O and delta D values extend over an area of at least 1600 km(2). The Chinese Continental Scientific Drilling project has made it possible to investigate the depth of the Qinglongshan anomaly and to measure an O-isotope profile across a garnet peridotite body sandwiched between crustal rocks. New O-isotope analyses of minerals separated from drill core gneisses, eclogites, amphibolite, and quartzite verify that the Qinglongshan O-isotope anomaly extends to a depth of at least 432 in. Crustal rocks with unusually low PO form both the hanging- and foot-walls of a 100 m thick, fault-bounded, garnet peridotite body intersected by the drill. Minerals of the garnet peridotite body have delta(18)O values indistinguishable from mantle nodules and megacrysts. The garnet peridotites may have originated from enriched mantle sources in sub-cratonic lithosphere, isolated from mantle convection. This origin is consistent with the collision of the Archean Sino-Korean craton with the Yangtze plate, consequent subduction, and UHP metamorphism. The garnet peridotite was transported from the mantle and emplaced into UHP crustal rocks during Triassic subduction and cratonic collision."],["dc.identifier.doi","10.2138/am.2005.1650"],["dc.identifier.isi","000229305300009"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/51192"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Mineralogical Soc Amer"],["dc.publisher.place","Washington"],["dc.relation.conference","Annual Meeting of the Geological-Society-of-America"],["dc.relation.eventlocation","Seattle, WA"],["dc.relation.issn","0003-004X"],["dc.title","Oxygen isotope geochemistry of rocks from the pre-pilot hole of the Chinese Continental Scientific Drilling Project (CCSD-PPH1)"],["dc.type","conference_paper"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","429"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Contributions to Mineralogy and Petrology"],["dc.bibliographiccitation.lastpage","442"],["dc.bibliographiccitation.volume","153"],["dc.contributor.author","Gao, Yongjun"],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Hellebrand, Eric"],["dc.contributor.author","von der Handt, Anette"],["dc.contributor.author","Snow, Jonathan E."],["dc.date.accessioned","2018-11-07T11:03:27Z"],["dc.date.available","2018-11-07T11:03:27Z"],["dc.date.issued","2007"],["dc.description.abstract","Major and trace element profiles of clinopyroxene grains in oceanic gabbros from ODP Hole 735B have been investigated by a combined in situ analytical study with ion probe, and electron microprobe. In contrast to the homogeneous major element compositions, trace elements (REE, Y, Cr, Sr, and Zr) show continuous core to rim zoning profiles. The observed trace element systematics in clinopyroxene cannot be explained by a simple diffusive exchange between melts and gabbros along grain boundaries. A simultaneous modification of the melt composition is required to generate the zoning, although Rayleigh fractional crystallization modelling could mimic the general shape of the profiles. Simultaneous metasomatism between the cumulate crystal and the porous melt during crystal accumulation is the most likely process to explain the zoning. Deformation during solidification of the crystal mush could have caused squeezing out of the incompatible element enriched residual melts (interstitial liquid). Migration of the melt along grain boundaries might carry these melt out of the system. This process named as synkinematic differentiation or differentiation by deformation (Natland and Dick in J Volcanol Geotherm Res 110(3-4):191-233, 2001) may act as an important magma evolution mechanism in the oceanic crust, at least at slow-spreading ridges."],["dc.identifier.doi","10.1007/s00410-006-0158-4"],["dc.identifier.isi","000244687500005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/51624"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0010-7999"],["dc.title","Trace element zoning in pyroxenes from ODP Hole 735B gabbros: diffusive exchange or synkinematic crystal fractionation?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","Q10001"],["dc.bibliographiccitation.journal","Geochemistry Geophysics Geosystems"],["dc.bibliographiccitation.volume","13"],["dc.contributor.author","Gao, Y."],["dc.contributor.author","Vils, F."],["dc.contributor.author","Cooper, Kari M."],["dc.contributor.author","Banerjee, N."],["dc.contributor.author","Harris, Midori"],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Teagle, D. A. H."],["dc.contributor.author","Casey, J. F."],["dc.contributor.author","Elliott, Tim"],["dc.contributor.author","Laverne, C."],["dc.contributor.author","Alt, J. C."],["dc.contributor.author","Muehlenbachs, Karlis"],["dc.date.accessioned","2018-11-07T09:04:45Z"],["dc.date.available","2018-11-07T09:04:45Z"],["dc.date.issued","2012"],["dc.description.abstract","Bulk rock lithium and oxygen isotope compositions from ODP Site 1256 were analyzed to investigate the seawater circulation in the upper oceanic crust formed at the East Pacific Rise (EPR). The upper extrusive basalts have delta O-18 values from +6.1% to +9.2%, reflecting alteration of oceanic crust by seawater at low temperatures (<200-250 degrees C). Bulk rocks from the sheeted dike complex and plutonic section have overall lower delta O-18 values(+3.0 parts per thousand+5.5 parts per thousand). In the sheeted dike complex bulk rock delta O-18 values gradually decrease with depth, and then increase toward the fresh MORB delta O-18 value after reaching a minimum of +3.0% at similar to 1350 m below seafloor (mbsf). The entire sampled crust is dominated by rocks with low lithium contents relative to fresh MORBs except for a few localized Li enrichment. The upper volcanic zone is characterized by a spread of delta Li-7 from low to high values relative to average unaltered MORB values (delta Li-7 = +3.4 +/- 1.4%). The presence of rocks with low delta Li-7 values in the upper crust most likely indicates zones of upwelling of relatively hot (similar to 200-250 degrees C) hydrothermal fluids. In the sheeted dike complex, bulk rock delta Li-7 values show wide range of variation, but exhibit a general trend from enriched to depleted values at similar to 1280 mbsf and then return to that for fresh MORB within the upper tens of meters of the plutonic section at the bottom of the after reaching a minimum at similar to 1350 mbsf (delta Li-7 = -1.6 parts per thousand). The downhole pattern of delta Li-7 principally reflects variations in water-rock ratio (w/r) together with a downhole increase of temperature. Seawater flow in the upper volcanic zone is likely to be channeled with generally small but variable w/r ratios. The w/r ratios increase rapidly with depth in the lower volcanic section into the sheeted dike complex indicating water dominated pervasive hydrothermal flow due to intensive upwelling of hydrothermal fluids."],["dc.identifier.doi","10.1029/2012GC004207"],["dc.identifier.isi","000309612600001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25173"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Amer Geophysical Union"],["dc.relation.issn","1525-2027"],["dc.title","Downhole variation of lithium and oxygen isotopic compositions of oceanic crust at East Pacific Rise, ODP Site 1256"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","809"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","ACTA PETROLOGICA SINICA"],["dc.bibliographiccitation.lastpage","818"],["dc.bibliographiccitation.volume","21"],["dc.contributor.author","Zhang, Z. M."],["dc.contributor.author","Xiao, Y. L."],["dc.contributor.author","Shen, K."],["dc.contributor.author","Gao, Y. J."],["dc.date.accessioned","2018-11-07T11:01:17Z"],["dc.date.available","2018-11-07T11:01:17Z"],["dc.date.issued","2005"],["dc.description.abstract","Garnet porphyroblasts with complex growth zonation and mineral inclusion are recognized in the ultrahigh-pressure (UHP) eclogites from Donghai area, southern Sulu orogenic belt. By investigating of petrography and mineral chemistry, four metamorphic stages have been revealed. They are the prograde epidote-amphibolite facies, coesite-eclogite facies, retrograde quartz-eclogite facies and amphibolite facies metamorphism. Using the compositions of the mantle segment of porphyroblastic garnets (with the lowest Fe/Mg ratio) and adjacent omphacite inclusion, and the related geothermobarometers, P-T conditions of > 900 degrees C and 4.1 similar to 4.5GPa are estimated for the stage of UHP metamorphism. Combining with the P-T conditions of other stages of metamorphism, a clockwise P-T path are reconstructed. It is characterized by the prograde trajectory is parallel nearly to the segment of retrogression, and the early retrograde metamorphism with coupling of decompression with a temperature decrease. Preservation of the growth zoning of eclogitic garnets suggests that the UHP rocks have a short residence time before the retrograde metamorphism and have a very high uplift rate. A temperature decrease during the early retrograde metamorphism of the UHP eclogites may be another favorable condition for preservation of garnet growth zoning."],["dc.identifier.isi","000231179000020"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/51115"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Science Press"],["dc.relation.issn","1000-0569"],["dc.title","Garnet growth compositional zonation and metamorphic P-T path of the ultrahigh-pressure eclogites from the Sulu orogenic belt, eastern Central China."],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","15A"],["dc.bibliographiccitation.journal","Geochimica et Cosmochimica Acta"],["dc.bibliographiccitation.volume","66"],["dc.contributor.author","Gao, Y."],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Snow, Jonathan E."],["dc.date.accessioned","2018-11-07T10:14:51Z"],["dc.date.available","2018-11-07T10:14:51Z"],["dc.date.issued","2002"],["dc.format.extent","A262"],["dc.identifier.isi","000177423400507"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/40700"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.publisher.place","Oxford"],["dc.relation.issn","0016-7037"],["dc.title","Oxygen isotope profile of the lower ocean crust: an in-situ study by UV-laser-ablation oxygen isotope microprobe"],["dc.type","conference_abstract"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]