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| 懞嶳丂夒巎丂乮Masafumi
Murayama乯 |
仠嫵堢尋媶晹 帺慠壢妛宯 棟妛晹栧 嫵庼
仠戝妛堾 憤崌恖娫帺慠壢妛尋媶壢 棟妛愱峌/墳梡帺慠壢妛愱峌
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仭庡側尋媶僥乕儅 |
埨掕丒曻幩惈摨埵懱傪梡偄偨奀梞僐傾偺崅惛搙擭戙應掕偲屆娐嫬暅尦
摨埵懱傪梡偄偨棨堟-奀堟偵偍偗傞暔幙弞娐偺夝柧 |
仭扴摉島媊 |
抧媴壢妛奣榑I乮嫟捠嫵堢乯
奀梞抧幙妛乮棟妛晹乯,
働乕僗僗僞僨傿IX乮棟妛晹乯
摨埵懱抧媴壢妛摿榑乮戝妛堾乯
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尋媶幒俹俼丒妛惗傊偺儊僢僙乕僕
埨掕丒曻幩惈摨埵懱傪梡偄偰丆奀梞 僐傾傗懲愊暔傗奀悈側偳偺擭戙應掕傪峴偄丆奀梞屆娐嫬偺暅尦傪峴偭偰偄傞丏擭戙應掕偼丆懠偺奀堟偐傜嵦庢偝傟偨奀梞僐傾傗昘彴僐傾丆屛徖僐傾側偳偲崅惛搙側懳斾傪峴偆忋偱昁梫晄壜寚偱偁傞丏夁嫀偵丆僌儘乕僶儖傗儘乕僇儖偵婲偙偭偨娐嫬僀儀儞僩偺摨帪惈傗慜屻娭學傪柧傜偐偵偡傞偙偲偑弌棃傞丏
傑偨丆摨埵懱偼丆抧媴忋偱婲 偙傞儅僋儘偐傜儈僋儘儗儀儖偺暔幙弞娐傪夝柧偡傞忋偱婱廳側僣乕儖偵側傞丏椺偊偽丆抧媴壏抔壔僈僗偺侾偮偲偟偰抦傜傟偰偄傞擇巁壔扽慺 (CO2乯偑丆戝婥寳丆悈寳
乮揤悈傗壨愳悈丆奀梞悈乯丆抧寳丆惗暔寳側偳偺憡屳偺弞娐僔僗僥儉偺拞偱偳偺傛偆 偵堏摦丒奼嶶丒挋憼偝傟偰偄傞偺偐傪夝柧偱偒傞丏嬤擭丆揤慠帒尮偲偟偰拲栚傪梺傃
偰偄傞儊僞儞僴僀僪儗乕僩偺惗惉婲尮傕丆偦偺扽慺摨埵懱斾偐傜乽惗暔敪峺婲尮乿側偺偐丆抧壓怺晹桼棃偺乽擬暘夝婲尮乿側偺偐摿掕偡傞偙偲偑壜擻偱偁傞丏
埲忋偺傛偆偵丆條乆側庬椶偺埨掕丒曻幩惈摨埵懱傪巊偭偨乽摨埵懱抧媴壔妛乿偼丆抧媴壢妛丆摿偵娐嫬抧媴壢妛偺彅栤戣偵戝偒偔峷專偟偰偄傞丅 |
仭幮夛妶摦側偳 |
擔杮抧幙妛夛丂戙媍堳丆
擔杮屆惗暔妛夛丂峴帠埾堳,
幒屗僕僆僷乕僋悇恑嫤媍夛丂塣塩埾堳
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仭懖嬈戝妛媦傃戝妛堾 |
崅抦戝妛棟妛晹抧妛壢懖嬈
崅抦戝妛戝妛堾棟妛宯尋媶壢抧幙妛愱峌廋巑壽掱廋椆
搶嫗戝妛戝妛堾棟妛宯尋媶壢攷巑壽掱廋椆 丂攷巑 (棟妛)
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仭強懏妛夛 |
傾儊儕僇暔棟妛楢崌妛夛 (AGU乯丆 擔杮抧媴榝惎壢妛楢崌丆擔杮抧幙妛夛丆
擔杮抧媴壔妛夛丆擔杮戞巐婭妛夛丆擔杮屆惗暔妛夛 |
仭庡側嬈愌 |
仠Latitudinal and downcore (0-750 ka) changes in n-alkane chain lengths in the eastern equatorial Pacific, Quaternary Research, 73, 573-582, doi:10.1016/j.yqres.2010.01.001, 2010乮嫟挊乯
仠Evidence for tropical South Pacific climate change during the Younger Dryas and the B?lling-Aller?d from geochemical records of fossil Tahiti corals, Earth Planet. Sci. Lett., 288, 96-107, doi:10.1016/j.epsl.2009.09.011. 2009乮嫟挊乯
仠The 1,500-year climate oscillation in the mid-latitude North Pacific during the Holocene, Geology, 37, 591-594; doi: 10.1130/G25667A., 2009乮嫟挊乯
仠Late Quaternary planktic foraminifer fauna and monsoon upwelling records from the western South China Sea, near the Vietnam margin (IMAGESMD012394), Terr. Atmos. Ocean. Sci., 19, 347-363, doi: 10.3319/TAO. 2008.19.4.347 (IMAGES), 2008乮嫟挊乯
仠Profiles of volumetric water content in fault zones retrieved from hole B of the Taiwan Chelungpu-fault Drilling Project (TCDP), Geophys. Res. Lett., 35, L01305, doi:10.1029/2007GL032158, 2008. 乮嫟挊乯
仠Truncated flame structure within deposit of the Indian Ocean Tsunami: evidence of syn-sedimentary deformation. Marine Geology, 54, 131-144, 2007乮嫟挊乯
仠Standing stock of deep-sea metazoan meiofauna in the Sulu Sea and adjacent areas. Deep Sea Research II, 54, 131-144, 2007乮嫟挊乯
仠Spatial and temporal sea-surface temperatures in the eastern equatorial Pacific over the past 150 kyr, Geophysical Research Letters, Vol. 33, L13605, doi:10.1029/2006GL025948. 2006乮嫟挊乯
仠High magnetic susceptibility of fault gouge within Taiwan Chelungpu-fault: Nondestructive continuous measurements of physical and chemical properties in fault rocks recovered from Hole B, TCDP. Geophysical Research Letters, 33, L15303, doi:10.1029/2006GL026133.2006乮嫟挊乯
仠Long term Aleutian Low dynamics and obliquity-controlled oceanic primary production in the mid-latitude western North Pacific (Core MD01-2421) during the last 145,000 years. Global Planet. Change, 53(1-2), 21-28, 2006乮嫟挊乯
仠Paleoceanographic change off central Japan since the last 144,000 years based on high-resolution oxygen and carbon isotope records. Global Planet Change, 53, 5-20, 2006乮嫟挊乯
仠Foraminiferal oxygen isotope stratigraphy and high-resolution organic carbon, carbonate records from the Okinawa Trough (IMAGES MD012404 and ODP Site 1202), Terr. Atmos. Ocean. Sci., 16, 57-73, 2005乮嫟挊乯
仠Fidelity of d18O as a proxy for sea surface temperature: Influence of variable coral growth rates on the coral Porites lutea from Hainan Island, China, Geochem. Geophys. Geosyst., 6, Q09017, doi:10.1029/2005GC000966., 2005乮嫟挊乯
仠North and south migrations of frontal zones during the past 40 kyr in the Kuroshio亅Oyashio transition area, Geochemistry Geophysics Geosystems, vol.5, 1-16, 2004乮嫟挊乯
仠Sea surface temperature and salinity changes in the northwest Pacific since the last glacial maximum, Journal of Quaternary Science, 19(4), 335-346, 2004乮嫟挊乯
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