(1. School of Earth Science and Geological Engineering,Sun Yat-sen University,Guangzhou 510275,China;
2. Earth Observatory of Singapore,Nanyang Technology University,Singapore 639798,Singapore;
3. College of Ocean and Earth Science,Xiamen University,Xiamen 361005,China)
CHEN Cong,WAN Qiuchi,ZHENG Zhuo,YU Fengling,A Switzer,WAN Yixing.. Late Quaternary Sediment Stratigraphy and Marine Cycles in
the Pingtan Island, Fujian Province
[J].TROPICAL GEOGRAPHY, 2016, 36(3): 406-416.
[1] CHAPPELL J,SHACKLETON N J.Oxygen isotopes and sea level [J].Nature,1986,324(6093):134-140.[2] CHAPPELL J.Oxygen isotopes,ice volume and sea level[J].Quaternary Science Reviews,1987,6(S3/4):183-190.[3] WAELBROECK C,LABEYRIE L,MICHEL E,DUPLESSY J C,MCMANUS J F,LAMBECK K,BALBON E,LABRACHERIE M.Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records[J].Quaternary Science Reviews,2002,21(S1/3):295-305.[4] BARD E,HAMELIN B,FAIRBANKS R G.U-Th ages obtained by mass spectrometry in corals from Barbados:sea level during the past 130,000 years[J].Nature,1990,346(6283):456-458.[5] CHAPPELL J,OMURA A,ESAT T,MCCULLOCH M,PANDOLFI J,OTA Y,PILLANS B.Reconciliation of late quaternary sea levels derived from Coral Terraces at Huon Peninsula with Deep Sea Oxygen isotope records[J].Earth and Planetary Science Letters,1996,141(1):227-236.[6] LAMBACK K,CHAPPELL J.Sea level change through the last glacial cycle[J].Sciense,2001,292(5517):679-686.[7] LAMBACK K,ESAT T M,EMMA-KATE P.Links between climate and sea level for the past three million years[J].Nature,2002,419(6903):199-206.[8] SIDDALL M,ROHLING E J,ALMOQI-LABIN A,HEMLEBEN CH,MEISCHNER D,SCHMELZER I,SMEED D A.Sea-level fluctuations during the last glacial cycle[J].Nature,2003,423(6942):853-858.[9] 杨怀仁,陈西庆.中国东部第四纪海面升降、海侵海退与岸线变迁[J].海洋地质与第四纪地质,1985,5(4):59-80. [10] 蔡爱智,龚金美.海坛岛芦洋浦平原的海进沙与风沙层序[J].应用海洋学学报,1992,11(2):112-117. [11] 蓝东兆,张维林.晚更新世以来台湾海峡西部的海侵及海平面变化[J].海洋学报,1993,15(4):77-84.[12] 王绍鸿,杨建明,曾从盛,吴学忠,俞鸣同.福建沿海晚更新世以来的海平面变化[J].台湾海峡,1994,13(2):166-175. [13] 蓝东兆,于永芬,陈承惠,谢在团.福州盆地晚更新世海侵及全新世海面波动的初步研究[J].海洋地质与第四纪地质,1986,6(3):103-111. [14] 杨建明.福建沿岸晚更新世末次海侵及其海平面的变化[J].海洋科学,1988(5):5-9. [15] 曾从盛.福建晚更新世海侵问题探讨[J].热带海洋学报,1993,12(1):39-45. [16] 杨建明.闽江口晚第四纪海侵地层的研究[J].福建师范大学学报(自然科学版),1993,9(1):86-90. [17] 周定成,孙全,许志峰.台湾海峡西部海域晚更新世3次“海侵”依据的探讨[J].应用海洋学学报,2011,30(3):324-329.[18] 王雨灼.福建省第四纪地层的划分[J].福建地质,1990,9(4):289-306. [19] 陈方.海坛岛第四纪地层及其沉积环境演变[J].海洋通报,1996,15(5):53-60. [20] 陈方.海坛岛的地貌及其发育演变[J].海洋通报,1994,13(6):60-66. [21] 赵绍华.平潭岛附近海域全新世以来沉积特征及古气候变化研究[D].厦门:国家海洋局第三海洋研究所,2012:7-15.[22] 温小浩,李保生,孟洁,杨庆江,郑琰明,牛东风,王丰年,蔡瑜杭.150~20 ka BP福建东部平潭岛海岸风成沉积的粒度特征及其环境意义[J].中国沙漠,2015,35(6):1473-1482.[23] UDDEN J A.Mechanical composition of clastic sediments[J].Geological Society of America Bulletin,1914,25:655-744.[24] WENTWORTH C K.A scale of grade and class terms for clastic sediments[J].Journal of Geology,1922,30(5):377-392.[25] FOLK R L,WARD W C.Brazos River bar [Texas]:a study in the significance of grain size parameters[J].Journal of Sedimentary Research,1957,27(1):3-26.[26] REIMER P J,BAILLIE M G L,BARD E,BAYLISS A,BECK J W,BLACKWELL P G.IntCal09 and Marine09 radiocarbon age calibration curves,0-50,000 years cal BP[J].Radiocarbon,2009,51(4):1111-1150.[27] FUCHS M,STRAUB J,Z?LLER L.Residual luminescence signals of recent river flood sediments:A comparison between quartz and feldspar of fine-and grain-sized sediments[J].Ancient Tl,2005,23(1):25-30.[28] HONG D G,MAN S C,HAN J H,CHEONG C S.Determination of sedimentation rate of a recently deposited tidal flat,western coast of Korea,using IRSL dating[J].Quaternary Science Reviews,2003,22(22):1185-1189.[29] MAUZ B,BAETEMAN C,BUNGENSTOCK F,PLATER A J.Optical dating of tidal sediments:Potentials and limits inferred from the North Sea coast[J].Quaternary Geochronology,2010,5(6):667-678.[30] KIM J C,CHANG T S,YI S,HONG S S,NAHM W H.OSL dating of coastal sediments from the southwestern Korean Peninsula:A comparison of different size fractions of quartz[J].Quaternary International,2014,384:82-90.[31] LISIECKI L E,RAYMO M E.A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records[J].Paleoceanography,2005,20(1):1-16.[32] 类彦立,李铁刚.奥茅卷转虫Ammonia aomoriensis(Asano,1951)与毕克卷转虫Ammonia beccarii(Linnaeus,1758)(有孔虫)的分类学以及在黄东海分布的温盐深特征比较研究[J].微体古生物学报,2015,32(1):1-19. [33] ZONG Y.Mid-Holocene sea-level highstand along the Southeast Coast of China[J].Quaternary International,2004,117(3):55–67.[34] 赵泉鸿,汪品先.中国浅海现代介形虫的数量和属种分布[J].海洋与湖沼,1988,19(6):553-561. [35] 刘春莲,Franz T Fursich,董艺辛,车晓光,陈亮,庄畅.珠江三角洲PRD05孔的高分辨率介形类记录与晚第四纪古环境重建[J].古地理学报,2008,10(3):313-322.[36] 王建,柏春广,徐永辉.江苏中部淤泥质潮滩潮汐层理成因机理和风暴沉积判别标志[J].沉积学报,2006,24(4):562-569.[37] 胡凡根,李志忠,靳建辉,赵倩,张辉,王贤立,夏菁.福建东部海坛岛老红砂敏感粒度组分对东亚冬季风演变的响应[J].中国沙漠,2013,33(2):443-452.[38] 黄镇国,宗永强.应用粒度参数区分沉积相——以珠江三角洲为例[J].热带地理,1982,2(2):37-42.[39] 唐丽,董玉祥.华南海岸现代风成沙与海滩沙的粒度特征差异[J].中国沙漠,2015,35(1):14-23.[40] 俞鸣同,张红艳,龚正权,陈有喜,王佳韡,张熠,胡绍洁,吴惠.福建平潭青峰老红砂中季风组分以及形成期研究[J].地理科学, 2014,34(3):352-357. [41] 巫锡良.福建沿海泥炭的成因分析[J].热带地理,1987,3(3):219-227.[42] 黄镇国,张伟强,蔡福祥,徐起浩.华南末次冰期盛期最低海面问题[J].地理学报,1995,50(5):385-393.[43] 施雅风,孔昭宸,王苏民,唐领余,王富葆,姚檀栋,赵希涛,张丕远,施少华.中国全新世大暖期的气候波动与重要事件[J].中国科学(B辑:化学生命科学地学),1992,22(12):1300-1308. [44] 张伟强,黄镇国.台湾沿岸全新世海平面波动[J].热带地理,1996,16(3):226-235.