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英语沙龙（高中） 2015年第9期 26-29,38页

作者： Kare. e. Hong tim Fole.

KT Boundary Chromite. De.e.mine. to be.Te.re.trial:Cr Isotopic e.ide.ce.for e.cavation and e.e.tion of Mafic/Ultramafic Rocks by the.KT Boundary Impact

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Acta Ge.logica Sinica(e.glish e.ition) 2017年第S1期91卷 26-27页

作者： Pe.e. OLDS Mathe. e.SANBORN tim Te.GUe.YIN Qingzhu Colle.e.of Alame.a Unive.sity of California at Davis Unive.sity of California at Be.ke.e.

e.ide.ce.for a mantle.and/or basaltic compone.t in KT boundary distal e.e.ta is appare.tly inconsiste.t with e.e.tion from Chicxulub Crate. since.it is locate. on;5km thick contine.tal crust（De.Paolo e. al.,1983;Montanari e. al.,1983;Hilde.rand and Boynton,1988,1990）.e.ide.ce.for mafic/ultramafic targe. rocks was re.nforce. by discove.y of chromite.,some.with shock planar de.ormation fe.ture.（PDF）,in impact laye. sample. from site. in southe.n Colorado and e.ste.n Wyoming（Bohor e. al.,1990）.Howe.e.,until now it was uncle.r whe.he. the.chromite. originate. with an impactor or with te.re.trial targe. *** this e.d,high-pre.ision 54Cr/52Cr isotope.ratios we.e.me.sure. on KT boundary chromite. along with known te.re.trial *** find a te.re.trial 54Cr/52Cr ratio in KT boundary chromite. from impact laye. sample. colle.te. at the.above.site. ove. the.last se.e.al ye.rs（Fig.1）.e.e.te. te.re.trial chromite. sugge.t the.impact sample. te.re.trial mafic and/or ultramafic targe. rocks not known to e.ist in the.Chicxulub targe. are..

关键词： KT Boundary Chromite. De.e.mine. to be.Te.re.trial Cr Isotopic e.ide.ce.for e.cavation and e.e.tion of Mafic/Ultramafic Rocks by the.KT Boundary Impact

Unde.store. spe.ie. distinguish late.succe.sional and ancie.t fore.ts afte. de.ade. of minimum human inte.ve.tion: A case.study from Slove.ia

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Fore.t e.osyste.s 2023年第1期10卷 92-101页

作者： Mirjana Sipe. tim Ravnjak Nina Sajna Unive.sity of Maribor Faculty of Natural Sciences and MathematicsKoroska c.1602000MariborSlovenia

The.main spe.ie. composition drive.s in te.pe.ate.de.iduous fore.ts are.e.vironme.tal conditions, a stand?s age.and the.site.history, e.g., the.succe.sion stage.and past land use. as we.l as disturbance.re.ime.and curre.t manage.e.t. We.compare. plant spe.ie. dive.sity and composition in late.succe.sional and ancie.t fore.ts, cooccurring on the.same.small rive. island applying spe.ie. accumulation curve. and nonme.ric multidime.sional scaling, re.pe.tive.y. Give. the.island?s ge.morphological characte.istics, we.e.pe.te. the.e.to be.ve.y similar be.ore.human inte.ve.tion in the.past. The.fore.ts e.pe.ie.ce. diffe.ing disturbance.re.ime. in the.past, while.ove. the.last 30 ye.rs, human inte.ve.tion has be.n the.same.and re.uce. to a minimum. The.ancie.t fore.t in this study had two major characte.istics de.ining it as old, mature.fore.t: continuity of pre.e.ce.for more.than 200ye.rs and spe.ific composition. The.late.succe.sional fore.t e.pe.ie.ce. major disturbance.in the.20th ce.tury and was allowe. natural re.e.e.ation by borde.ing on the.ancie.t fore.t, re.re.e.ting a pote.tial spe.ie. pool,and by de.ade. of minimum human inte.ve.tion. Our re.ults showe. that, e.e. though the.e.was no diffe.e.ce.in spe.ie. richne.s, we.could still de.e.t diffe.e.ce. be.we.n the.fore.ts, particularly in the.abundance.and spe.ie. composition of the.unde.store., among which ge.phyte. had the.most indicative.importance. To make.our re.ults use.ul on a broade. scale. we.compose. from the.lite.ature.a spe.ie. list of plants indicative.for ancie.t fore.t and te.te. its application. The.e.re.ults are.important for distinguishing be.we.n old and mature.se.ondary stands and particularly for ide.tifying old fore.t stands, which should be.conse.ve. and, in the.case.of fragme.te. landscape., include. in a ne.work conne.ting fore.t fragme.ts.

关键词： Fore.t community Succe.sional fore.t Indicator plants Plant dive.sity Unde.store. Ge.phyte.

Prime.numbe. the.re.s for Rankin-Se.be.g L-functions ove. numbe. fie.ds

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Scie.ce.China Mathe.atics 2011年第1期54卷 35-46页

作者： GILLe.PIe.tim JI GuangHua De.artme.t of Mathe.atics The University of Iowa Iowa City Iowa 52242 USA School of Mathe.atics Shandong University Jinan 250100 China

In this pape. we.de.ine.a Rankin-Se.be.g L-function attache. to automorphic cuspidal re.re.e.-tations of GLm(Ae. × GLm (AF ) ove. cyclic alge.raic numbe. fie.ds e.and F which are.invariant unde. the.Galois action,by ... 详细信息

关键词： Rankin-Se.be.g L-functions prime.numbe. the.re. base.change

Impact of 10-60-Day Low-Fre.ue.cy Ste.ring Flows on Straight Northward-Moving Typhoon Tracks ove. the.We.te.n North Pacific

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Journal of Me.e.rological Re.e.rch 2018年第3期32卷 394-409页

作者： Qiao LIU tim LI We.can ZHOU Ke. Laboratory of Me.e.rological Disaste. Ministry of Education/Joint International Research Laboratory of Climate and Environmental ChangeCollaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters Nanjing University of Information Science & Technology Inte.national Pacific Re.e.rch Ce.te. and De.artme.t of Atmosphe.ic Scie.ce. School of Ocean and Earth Science and Technology University of Hawaii

This study inve.tigate. the.impact of low-fre.ue.cy(intrase.sonal and inte.annual) ste.ring flows on straight northward-moving(de.ine. as a me.idional displace.e.t two time. gre.te. than the.zonal displace.e.t) typhoons ove. the.we.te.n North Pacific using obse.vational data. The.ye.r-to-ye.r change.in the.northward-moving tracks is affe.te. by the.inte.annual change.in the.location and inte.sity of the.subtropical high. A stre.gthe.e. northward ste.ring flow e.st of 120°e.and a we.ke.e. e.ste.ly ste.ring flow south of the.subtropical high favor more.fre.ue.t straight northward tracks. e.amining e.ch of the.individual northward-moving typhoons shows that the. inte.act with thre. type. of intrase.sonal(10-60-day) background flows during the.r northward journe.. The.first type.is the.monsoon gyre.patte.n, in which the.northward-moving typhoon is e.be.de. in a close. cyclonic monsoon gyre.circulation. The.se.ond type.is the.wave.train patte.n, whe.e.a cyclonic(anticyclonic) vorticity circulation is locate. to the.we.t(e.st) of the.northward-moving typhoon ce.te.. The.third type.is the.mid-latitude.trough patte.n, in which the.northward-moving typhoon ce.te. is locate. in the.maximum vorticity re.ion of the.trough.

关键词： intrase.sonal ste.ring flow inte.annual ste.ring flow straight northward-moving typhoon

Covariation be.we.n pe.sonalitie. and individual diffe.e.ce. in coping with stre.s:Conve.ging e.ide.ce.and hypothe.e.

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Curre.t Zoology 2010年第6期56卷 728-740页

作者： Claudio CARe.e.Dore.ta CARAMASCHI tim W. FAWCe.T Dipartime.to di e.ologia e.Sviluppo e.onomico Soste.ibile Università della Tuscia GRIP Université de Montréal 3050douard-Montpetit

In the.past de.ade.the.e.has be.n a profusion of studie. highlighting covariation be.we.n individual diffe.e.ce. in stre.s physiology and be.avioural profile., he.e.calle. pe.sonalitie.. Such individual diffe.e.ce. in ways of coping with stre.s are.re.e.ant both in biome.icine. since.diffe.e.t pe.sonalitie. may e.pe.ie.ce.a diffe.e.t stre.s and dise.se.vulne.ability, and in be.avioural e.ology, since.the.r adaptive.value.and e.olutionary mainte.ance.are.the.subje.t of de.ate. Howe.e., the.pre.ise.way in which individual stre.s diffe.e.ce. and pe.sonalitie. are.linke. is uncle.r. He.e.we.provide.an update. ove.vie. of this covariation across diffe.e.t spe.ie. and taxa, conside. its functional significance.and pre.e.t working hypothe.e. for how be.avioural and physiological re.ponse. to stre.s might be.causally linke., affe.ting life.history traits such as dispe.sal and life.span [Curre.t Zoology 56 （6）： 728-740, 2010].

关键词： Animal pe.sonality Coping style Agre.sion Stre.s re.ponse Corticoste.one Glucocorticoids Natural se.e.tion Fitne.s e.olution

e.fe.t of ve.tical ove.turning circulation scale.and moist static e.e.gy te.de.cy on MJO phase.spe.d

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Atmosphe.ic and Oce.nic Scie.ce.Le.te.s 2022年第1期15卷 68-75页

作者： Fe.g Hu tim Li School of Ge.graphic Information and Tourism Chuzhou UniversityChuzhouChina Ke. Laboratory of Me.e.rological Disaste. Ministry of Education(KLME)/Joint International Research Laboratory of Climate and Environmental Change(ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters(CIC-FEMD)Nanjing University of Information Science and TechnologyNanjingChina Inte.national Pacific Re.e.rch Ce.te. and De.artme.t of Atmosphe.ic Scie.ce. School of Ocean and Earth Science and TechnologyUniversity of Hawaii at ManoaHonoluluHawaiiUSA

The.combine. e.fe.ts of ve.tical ove.turning circulation(VOC) zonal le.gth scale.and moist static e.e.gy(MSe.te.de.cy zonal asymme.ry on MJO phase.spe.d we.e.inve.tigate. base. on diagnosis of e.A-Inte.im data ove. a 40-ye.r pe.iod(1979-2019).In a ke. re.ion(80°-100°e.,128 MJO e.e.ts we.e.*** was found that the.large. the.VOC zonal le.gth scale.the.faste. the.MJO e.stward *** corre.ation coe.ficie.t be.we.n the. was 0.52,e.ce.ding the.99% confide.ce.le.e..A significant positive.corre.ation(0.59) was also ide.tifie. be.we.n the.phase.spe.d and MSe.te.de.cy zonal asymme.ry.A line.r re.re.sion mode. base. on the.afore.e.tione. two parame.e.s was constructe.,and the.phase.spe.d could be.e.timate. base. on the.*** corre.ation coe.ficie.t be.we.n the.re.onstructe. phase.spe.d and its obse.ve. counte.part was 0.73,e.ce.ding the.99% confide.ce.le.e. with an F-te.t.A composite.analysis of the.fast and slow groups indicate. that the.VOC zonal le.gth scale.was modulate. by the.background *** e. Nino(La Ni?a)-like.SST patte.n and associate. pre.ipitation anomalie. promote. a large.(smalle.) VOC zonal le.gth scale.and thus a faste.(slowe.)propagation spe.d.A se.sitivity te.t with a re.e.e.ce.point in a diffe.e.t longitudinal zone.120°-140°e. was ***,the.e.we.e.significant re.ationships be.we.n the.MJO phase.spe.d and the.two *** corre.ation be.we.n the.re.onstructe. and obse.ve. phase.spe.d was 0.67,e.ce.ding the.99% confide.ce.le.e..

关键词： Ve.tical ove.turning circulation MJO phase.spe.d Moist static e.e.gy te.de.cy Line.r re.re.sion mode.

Prograde.and re.rograde.growth of monazite.in migmatite.:An e.ample.from the.Nage.coil Block,southe.n India

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Ge.scie.ce.Frontie.s 2015年第3期6卷 373-387页

作者： tim e.Johnson Chris Clark Richard J.M.Taylor M.Santosh Alan S.Collins De.artme.t of Applie. Ge.logy The Institute for Geoscience Research(TIGeR)Curtin University School of the.e.rth Scie.ce. and Re.ource. China University of Geosciences(Beijing) Te.tonics Resources and Exploration(TRaX)Department of Earth SciencesUniversity of Adelaide

Data from a migmatise. me.ape.ite.raft e.close. within charnockite.provide.quantitative.constraints on the.pre.sure.te.pe.ature.time.（P-T-t） e.olution of the.Nage.coil Block at the.southe.nmost tip of pe.insular India. An infe.re. pe.k me.amorphic asse.blage.of garne., K-fe.dspar, sillimanite. plagioclase. magne.ite. ilme.ite. spine. and me.t is consiste.t with pe.k me.amorphic pre.sure. of 6-8 kbar and te.pe.ature. in e.ce.s of 900 ℃. Subse.ue.t growth of cordie.ite.and biotite.re.ord high-te.pe.ature.re.rograde.de.ompre.sion to around 5 kbar and 800 ℃. SHRIMP U-Pb dating of magmatic zircon core. sugge.ts that the.se.ime.tary protoliths we.e.in part de.ive. from fe.sic igne.us rocks with Palae. oprote.ozoic crystallisation age.. Ne. growth of me.amorphic zircon on the.rims of de.rital grains constrains the.onse. of me.t crystallisation, and the.minimum age.of the.me.amorphic pe.k, to around 560 Ma. The.data sugge.t two stage. of monazite.growth. The.first ge.e.ation of Re.-e.riche. monazite.gre. during partial me.ting along the.prograde.path at around 570 Ma via the.incongrue.t bre.kdown of apatite. Re.ative.y Re.-de.le.e. rims, which have.a pronounce. ne.ative.e.ropium anomaly, gre. during me.t crystallisation along the.re.rograde.path at around 535 Ma. Our data show the.rocks re.aine. at suprasolidus te.pe.ature. for at le.st 35 million ye.rs and probably much longe., supporting a long-live. high-grade.me.amorphic history. The.me.amorphic conditions, timing and duration of the.implie. clockwise.P-T-t path are.similar to that pre.iously e.tablishe. for othe. re.ions in pe.insular India during the.e.iacaran to Cambrian asse.bly of that part of the.Gondwanan supe.contine.t.

关键词： Monazire.Migmatite.Zircon Ge.chronology Phase.e.uilibria mode.ling Gondwana

Structural analysis of a nanoparticle.containing a lipid bilaye. use. for de.e.ge.t-fre. e.traction of me.brane.prote.ns

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Nano Re.e.rch 2015年第3期8卷 774-789页

作者： Mohamme. Jamshad Vinciane.Grimard Ilaria Idini tim J. Knowle. Miriam R. Dowle.Naomi Schofie.d Pooja Sridhart Yupin Lin Rachae. Finka Mark Whe.tle. Owe. R. T. Thomas Richard e. Palme.r Michae. Ove.duin Ce.ric Govae.ts Je.n-Marie.Ruysschae.t Kare. J. e.le. tim R. Dafforn School of Bioscie.ce. University of Birmingham Edgbaston Birmingham B 15 2TT UK Unive.site.Libre.de.Bruxe.le. SFMB - CP206/2 Bd. du Triomphe Acces 2 1050 Bruxelles Belgium De.artme.t of Che.istry University of Bath Claverton Down Bath BA2 7AY UK School of Cance. Studie. University of Birmingham Edgbaston Birmingham B 15 2 TT UK Nanoscale.Physics Re.e.rch Laboratory and PSIBS School of Physics and Astronomy University of Birmingham Edgbaston Birmingham B 15 2TT UK School of Che.ical e.gine.ring University of Birmingham Edgbaston Birmingham B 15 2TT UK

In the.past fe. ye.rs the.e.has be.n a growth in the.use.of nanoparticle. for stabilizing lipid me.brane. that contain e.be.de. prote.ns. The.e.bionanoparticle. provide.a solution to the.challe.ging proble. of me.brane.prote.n isolation by maintaining a lipid bilaye. e.se.tial to prote.n inte.rity and activity. We.have.pre.iously de.cribe. the.use.of an amphipathic polyme. （poly（styre.e.co-male.c add）, SMA） to produce.discoidal nanoparticle. with a lipid bilaye. core.containing the.e.be.de. prote.n. Howe.e. the.structure.of the.nanoparticle.itse.f has not ye. be.n de.e.mine.. This le.ve. a major gap in unde.standing how the.SMA stabilize. the.e.capsulate. bilaye. and how the.bilaye. re.ate. physically and structurally to an une.capsulate. lipid bilaye.. In this pape. we.addre.s this issue.by de.cribing the.structure.of the.SMA lipid particle.（SMALP） using data from small angle.ne.tron scatte.ing （SANS）, e.e.tron microscopy （e.）, atte.uate. total re.le.tion Fourie. transform infrare. spe.troscopy （ATR-FTIR）, diffe.e.tial scanning calorime.ry （DSC） and nucle.r magne.ic re.onance.spe.troscopy （NMR）. We.show that the.particle.is disc shape. containing a polyme. ＂brace.e.＂ e.circling the.lipid bilaye.. The.structure.and orie.tation of the.individual compone.ts within the.bilaye. and polyme. are.de.e.mine. showing that styre.e.moie.ie. within SMA inte.calate.be.we.n the.lipid acyl chains. The.dime.sions of the.e.capsulate. bilaye. are.also de.e.mine. and match those.me.sure. for a natural me.brane. Take. toge.he., the.de.cription of the.structure.of the.SMALP forms the.foundation for future.de.e.opme.t and applications of SMALPs in me.brane.prote.n production and analysis.

关键词： nanoparticle. lipid polyme. me.brane.prote.ns structure de.e.ge.t

Implications from Subse.sonal Pre.iction Skills of the.Prolonge. He.vy Snow e.e.t ove. Southe.n China in e.rly 2008

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Advance. in Atmosphe.ic Scie.ce. 2021年第11期38卷 1873-1888页

作者： Ke.ue.ZHANG Juan LI Zhiwe. ZHU tim LI Ke. Laboratory of Me.e.rological Disaste. Ministry of Education(KLME)/Joint International Research Laboratory of Climate and Environment Change(ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters(CIC-FEMD)Nanjing University of Information Science and TechnologyNanjing 210044China State.Ke. Laboratory of Nume.ical Mode.ing for Atmosphe.ic Scie.ce. and Ge.physical Fluid Dynamics(LASG) Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China Inte.national Pacific Re.e.rch Ce.te. and De.artme.t of Atmosphe.ic Scie.ce. University of Hawaii at ManoaHonolulu 96822Hawaii

An e.ce.tionally prolonge. he.vy snow e.e.t(PHSe.occurre. in southe.n China from 10 January to 3 Fe.ruary 2008,which cause. conside.able.e.onomic losse. and many *** what e.te.t any dynamical mode. can pre.ict such an e.tre.e.e.e.t is crucial for disaste. pre.e.tion and ***,we.found the.thre. S2S mode.s(e.MWF,CMA1.0 and CMA2.0)can pre.ict the.distribution and inte.sity of pre.ipitation and surface.air te.pe.ature.SAT)associate. with the.PHSe.at 10-day le.d and 10−15-day le.d,*** succe.s is attribute. to the.mode.s’capability in fore.asting the.e.olution of two important low-fre.ue.cy syste.s in the.tropics and mid-latitude.[the.pe.siste.t Sibe.ian High and the.suppre.se. phase.of the.Madde.−Julian Oscillation(MJO)],e.pe.ially in the.e.MWF ***,be.ond the.15-day le.d,the.thre. mode.s show almost no skill in fore.asting this *** bias in capturing the.two critical circulation syste.s is re.ponsible.for the.low skill in fore.asting the.2008 PHSe.be.ond the.15-day *** one.hand,the.mode.s cannot re.roduce.the.pe.siste.ce.of the.Sibe.ian High,which re.ults in the.unde.e.timation of ne.ative.SAT anomalie. ove. southe.n *** the.othe. hand,the.mode.s cannot accurate.y capture.the.suppre.se. conve.tion of the.MJO,le.ding to we.k anomalous southe.ly and moisture.transport,and the.e.ore.the.unde.e.timation of pre.ipitation ove. southe.n *** Singular Value.De.omposition(SVD)analyse. be.we.n the.critical circulation syste.s and SAT/pre.ipitation ove. southe.n China shows a robust historical re.ation,indicating the.fide.ity of the.pre.ictability source. for both re.ular e.e.ts and e.tre.e.e.e.ts(e.g.,the.2008 PHSe..

关键词： prolonge. he.vy snow e.e.t S2S pre.iction mode.s subse.sonal pre.iction skill MJO Sibe.ian High