Sedimentary and environment evolutionary records of the southern Lixiahe area in the Subei Plain during Holocene
-
摘要:
通过对里下河南部泰州地区PM4剖面样品的微体古生物鉴定及粒度分析，结合AMS14C测年，探讨了该地区全新世以来沉积环境的演化。研究结果表明，全新世以来，该地区的沉积环境经历了湖相、滨海沼泽、海湾、瀉湖、湖相5个阶段。11900~4850cal.aBP：沉积物颜色为灰色-灰黑色，颗粒较细，为极正偏的尖峰态，水动力条件较弱，不含有孔虫和介形虫，为湖相沉积；4850~4250cal.aBP：水动力增强及粗颗粒沉积物增加，含有少量有孔虫，为滨海沼泽；4250~4050cal.aBP：砂质成分急剧增加，含有大量有孔虫，位于黄桥沙坝的北汊道内，为海湾沉积；4050~1850cal.aBP：粒度变细，水动力减弱，含有少量有孔虫及介形虫，为瀉湖沉积；1850~0cal.aBP：粒度变细，分选变好，水动力条件较弱，不含有孔虫，含有少量介形虫，为湖相沉积。
Abstract:The PM4 section, 3.4 m in thickness, occurs in the south of the Lixiahe Plain (32°34′N, 119°56′E). The section lithologically consists of silt, clay and sand. 170 samples every 2cm are taken for grain size analysis in addition to 7 samples for AMS 14C dating and 86 samples every 4 cm for determination of foraminifera and ostracoda species. 5 stratigraphic units are identified from bottom to top according to the foraminifera and ostracoda assemblages, median grain size and other grain size parameters. The sediments from depth of 1.4~3.4 m or 11900~4850 cal.aBP are dominated by gray-black lacustrine deposits consisting mainly of silt, 83.9% on average. Clay and sand concentrations are 14.9% and 1.2%, respectively on average.Neither foraminifera nor ostracoda has been found. From the depth range of 1.1~1.4 m or 4850~4250 cal.aBP in age, the increase in silt and sand content indicates that water dynamics was intensified comparing to that in previous stage, suggesting an environment of coastal swamps. From 4250~4050 cal.aBP (1.14~0.98 m), sand sharply increased to 11.7%~15.3%, or 13.9% on average, indicating that the depositional environment was a bay behind the north branch of the Huangqiao sand bar. From 4050~1850 cal.aBP or from 0.98~0.68 m in depth, silt increased to 82.9%~88.6%, 86.3% on average, indicating that the hydrodynamics was weakened in that region. Foraminifera was rare, suggesting a lagoonal facies. During the period of 1850~0 cal.aBP (0.68~0 m): sand input was reduced to 1.0%~11.1% or 3.2% on average. No foraminifera is observed excluding small amount of ostracoda, suggesting a lacustrine environment.
-
Key words:
- grain size /
- micro-paleontology /
- sedimentary environment /
- Subei Plain
-
-
表 1 PM4剖面AMS14C年代序列及CAL. 7.1校正结果
Table 1. AMS14C dating results of PM4 section
样品号 岩性 深度/cm 测年材料 AMS14C年龄/aBP 校正年龄/cal.aBP(2σ) PM4-1 灰色含粉砂黏土 60 腐殖质 1365 ± 30 1299 ± 39 PM4-2 灰黄色粉砂 78 有机质 5350 ± 50 6110 ± 112 PM4-3 灰黄色粉砂 100 有机质 3810 ± 35 4194 ± 106 PM4-4 灰色粉砂质黏土 112 有机质 4860 ± 40 5619.5 ± 41.5 PM4-5 灰色粉砂质黏土 122 有机质 3870 ± 35 4321 ± 95 PM4-6 灰色粉砂质黏土 136 有机质 4145 ± 35 4698.5 ± 128.5 PM4-7 深灰-灰黑色含粉砂黏土 338 腐殖质 10280 ± 50 11982 ± 209 
下载: 导出CSV
-
[1] 凌申.全新世以来里下河地区古地理演变[J].地理科学, 2001, 21(5):474-479. doi: 10.3969/j.issn.1000-0690.2001.05.017
LING Shen. Palaeographic changes of the Lixiahe district since the Holocene [J]. Scientia Geographica Sinica, 2001, 21(5):474-479. doi: 10.3969/j.issn.1000-0690.2001.05.017
[2] 王靖泰, 汪品先.中国东部晚更新世以来海面升降与气候变化的关系[J].地理学报, 1980, 35(4):299-312. doi: 10.3321/j.issn:0375-5444.1980.04.003
WANG Jingtai, WANG Pinxian. Relationship between sea-level changes and climatic fluctuations in east Chia since late Pleistocene[J]. Acta Geographica Sinica, 1980, 35(4):299-312. doi: 10.3321/j.issn:0375-5444.1980.04.003
[3] 杨競红, 王颖, 张振克, 等.苏北平原2.58 Ma以来的海陆环境演变历史—宝应钻孔沉积物的常量元素记录[J].第四纪研究, 2006, 26(3):340-352. doi: 10.3321/j.issn:1001-7410.2006.03.005
YANG Jinghong, WANG Ying, ZHANG Zhenke, et al. Major element records of land-sea interaction and evolution in the past 2.58 Ma from the Baoying borehole sediments, Northern Jiangsu plain, China[J]. Quaternary Sciences, 2006, 26(3):340-352. doi: 10.3321/j.issn:1001-7410.2006.03.005
[4] 舒强, 李才林, 赵志军, 等.苏北盆地浅钻沉积物磁化率与粒度记录的末次冰消期以来的环境变化[J].沉积学报, 2009, 27(1):111-117. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200901015
SHU Qiang, LI Cailin, ZHAO Zhijun, et al. The records of mass susceptibility and grain size for climate changes in Subei Basin during the last deglaciation[J]. Acta Sedimentologica Sinca, 2009, 27(1):111-117. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200901015
[5] 赵希涛, 鲁刚毅, 王绍鸿, 等.江苏建湖庆丰剖面全新世地层及环境变迁与海面变化的初步研究[J].科学通报, 1990, 35(4):285-288.
ZHAO Xitao, LU Gangyi, WANG Shaohong, et al. Study on the Holocene stratigraphy, environmental changes and sea level variations from the Qingfeng section, Jianhu County, Jiangsu Province[J]. Chinese Sciences Bulletin, 1990, 35(4):285-288.
[6] 赵希涛, 唐领余, 沈才明, 等.江苏建湖庆丰剖面全新世气候变迁和海面变化[J].海洋学报, 1994, 16(1):78-88. doi: 10.3321/j.issn:0253-4193.1994.01.004
ZHAO Xitao, TANG Lingyu, SHEN Caiming. Holocene climate and the change of sea level in Jianhu County, Jiangsu Province[J]. Acta Oceanologica Sinica, 1994, 16 (1):78-88. doi: 10.3321/j.issn:0253-4193.1994.01.004
[7] 凌申.苏北全新世海进与古砂堤研究[J].台湾海峡. 1994, 13(4):338-345. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400730522
LING Shen. Study on Holocene transgression and sandbars in North Jiangsu[J]. Journal of Oceanography in Taiwan Strait, 1994, 13(4):338-345. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400730522
[8] 凌申.全新世以来苏北平原古地理环境演变[J].黄渤海海洋, 1990, 8(4):23-25. http://www.cnki.com.cn/Article/CJFDTOTAL-HBHH199004003.htm
LING Shen. Changes of the palaeogeographic environment in north Jiangsu plains since the Holocene[J]. Journal of Oceanography of Huanghai &Bohai Seas, 1990, 8(4):23-25. http://www.cnki.com.cn/Article/CJFDTOTAL-HBHH199004003.htm
[9] 郭盛乔, 马秋斌, 张祥云, 等.里下河地区全新世自然环境变迁[J].中国地质, 2013, 40(1):341-351. doi: 10.3969/j.issn.1000-3657.2013.01.024
GUO Shengqiao, MA Qiubin, ZHANG Xiangyun, et al. Holocene environmental changes in Lixiahe area[J]. Geology in China, 2013, 40(1):341-351. doi: 10.3969/j.issn.1000-3657.2013.01.024
[10] 张景文, 李桂英, 赵希涛.苏北地区全新世海陆变迁的年代学研究[J].海洋科学, 1983, 7(6):8-11. http://www.cnki.com.cn/Article/CJFDTOTAL-HYKX198306002.htm
ZHANG Jingwen, LI Guiying, ZHAO Xitao. Chronological study of the Holocene sea-land shift in northern Jiangsu[J]. Marine Sciences, 1983, 7(6):8-11. http://www.cnki.com.cn/Article/CJFDTOTAL-HYKX198306002.htm
[11] 冯金顺, 孙磊, 葛云, 等.江苏省里下河(兴化-泰州)地区浅表沉积物特征及古地理环境演变[J].江苏地质, 2007, 31(2):101-107. http://d.old.wanfangdata.com.cn/Periodical/jsdz200702004
FENG Jinshun, SUN Lei, GE Yun, et al. On shallow sediment properties and paleographic environment Xinghua-Taizhou, Jiangsu[J], Jiangsu Geology, 2007, 31(2):101-107. http://d.old.wanfangdata.com.cn/Periodical/jsdz200702004
[12] 朱诚, 吴立, 李兰, 等.对江苏新石器时代海面变化问题的再认识[J].科学通报, 2016, 61(3):374-387. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201603013
ZHU Cheng, WU Li, LI Lan, et al. Recognition of sea-level change during the Neolithic period in the Jiangsu Area, East China[J]. Chinese Science Bulletin, 2016, 61(3):374-387. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201603013
[13] 陈冬梅, 穆桂金.不同沉积环境下沉积物的粒度分形特征的对比研究[J].干旱区地理, 2004, 27(1):47-51. doi: 10.3321/j.issn:1000-6060.2004.01.009
CHEN Dongmei, MU Guijin. Comparising study of grain-size fractal dimensions characteristics between several sediments with different forming environments[J]. Arid Land Geography, 2004, 27(1):47-51. doi: 10.3321/j.issn:1000-6060.2004.01.009
[14] 王中波, 杨守业, 张志珣, 等.东海陆架中北部沉积物粒度特征及其沉积环境[J].海洋与湖沼, 2012, 43(6):1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003
WANG Zhongbo, YANG Shouye, ZHANG Zhixun, et al. The grain size compositions of the surface sediments in the east China sea:indication for sedimentary environments[J]. Oceanologia et Limnologia Sinica, 2012, 43(6):1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003
[15] 王伟, 李安春, 徐方建, 等.北黄海表层沉积物粒度分布特征及其沉积环境分析[J].海洋与湖沼, 2009, 40(5):525-531. doi: 10.3321/j.issn:0029-814X.2009.05.001
WANG Wei, LI Anchun, XU Fangjian, et al. Distribution of surface sediments and sedimentary environment in the north Yellow sea[J]. Oceanologia et Limnologia Sinica, 2009, 40(5):525-531. doi: 10.3321/j.issn:0029-814X.2009.05.001
[16] 石学法, 申顺喜, 陈志华, 等.南黄海现代沉积环境及动力沉积体系[J].科学通报, 2001, 46(s1):1-6. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB2001S1000.htm
SHI Xuefa, SHEN Shunxi, CHEN Zhihua, et al. Modern sedimentary environments and dynamic depositional systems in the southern Yellow Sea[J]. Chinese Science Bulletin, 2001, 46(s1):1-6. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB2001S1000.htm
[17] 王飞飞, 王红, 刘健, 等.南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义[J].海洋地质与第四纪地质, 2011, 31(4):113-123. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=136e5baa-780d-4f41-ba14-ca1487dace19
WANG Feifei, WANG Hong, LIU Jian, et al. Late quaternary benthic forminifera of core SYS-0803 from the northwestern south Yellow sea and their paleoenviromental significance[J]. Marine Geology & Quaternary Geology, 2011, 31(4):113-123. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=136e5baa-780d-4f41-ba14-ca1487dace19
[18] 赵泉鸿, 翦知湣, 张在秀, 等.东海陆架泥质沉积区全新世有孔虫和介形虫及其古环境应用[J].微体古生物学报, 2009, 26(2):117-128. doi: 10.3969/j.issn.1000-0674.2009.02.002
ZHAO Quanhong, JIAN Zhimin, ZHANG Zaixiu, et al. Holocene bethic foraminifera and ostracodafrom the shelf mud area of the east China sea and their paleoenvironmental implications[J]. Acta Micropalaeontologica Sinica, 2009, 26(2):117-128. doi: 10.3969/j.issn.1000-0674.2009.02.002
[19] Li L, Zhu C, Lin L, et al. Evidence for marine transgression between 7500-5400BC at the Luotuodun Site in Yixing, Jiangsu Province[J]. Journal of Geographical Sciences, 2009, 19(6):671-680. doi: 10.1007/s11442-009-0671-2
[20] 蔡庆芳, 王飞飞, 印萍, 等.全新世以来长江口底栖有孔虫组合及古环境演化[J].海洋地质与第四纪地质, 2016, 36(6):175-184. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=e9f871c6-d2ce-4088-b98e-7996f2c7b202
CAI Qingfang, WANG Feifei, YIN Ping, et al. Subassemblages of benthic formaminifera and palaeoenvironmental implication in the Yangtze river estuary since Holocene[J]. Marine Geology & Quaternary Geology, 2016, 36(6):175-184. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=e9f871c6-d2ce-4088-b98e-7996f2c7b202
[21] Stuiver M, Reimer P J. A computer program for radiocarbon age calibration. Radiocarbon[J], 1986, 28(2B) :1022-1030. doi: 10.1017/S0033822200060276
[22] 鹿化煜, 苗晓东, 孙有斌.前处理步骤与方法对风成红黏土粒度测量的影响[J].海洋地质与第四纪地质, 2002, 22(3):129-135. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=3b2917cf-83e8-4a40-ba39-e4aefbd073d9
LU Huayu, MIAO Xiaodong, SUN Youbin. Pretreatment methods and their influences on grain-size measurement of aeolian "red clay" in north China[J]. Marine Geology & Quaternary Geology, 2002, 22(3):129-135. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=3b2917cf-83e8-4a40-ba39-e4aefbd073d9
[23] 鹿化煜, 安芷生.前处理方法对黄土沉积物粒度测量影响的实验研究[J].科学通报, 1997, 2(23):2535-2538. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199723016.htm
LU Huayu, AN Zhisheng. Pretreatment methods in loess-paleosol granulometry[J]. Chinese Science Bulletin, 1997, 42:237-240. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199723016.htm
[24] Clark M W. Some methods for statistical analysis of multimodal distributions and their application to grain-size data[J]. Mathematical Geology, 1976, 8(3):267-282. doi: 10.1007/BF01029273
[25] Blott S J, Pye K. GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments[J]. Earth Surface Processes and Landforms, 2001, 26(11):1237-1248. doi: 10.1002/esp.261
[26] Müller G, Förstner U. General relationship between suspended sediment concentration and water discharge in the Alpenrhein and some other rivers[J]. Nature, 1968, 217(5125):244-245. doi: 10.1038/217244a0
[27] Friedman G M, Sanders J E. Principles of sedimentology[M]. New York:Wiley, 1978:1-792.
[28] 闫晓洁, 胥勤勉, 范友良等.渤海湾西北岸HG01孔晚更新世以来的微体化石特征及沉积演化过程[J].第四纪研究, 2017, 37(1):97-107. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201701009
YAN Xiaojie, XU Qinmian, FAN Youliang, et al. Microfossil assemblages characteristics and sedimentary evolution of HG01 borehole in the northwest coast of Bohai Bay since Late Pleistocene[J]. Quaternary Sciences, 2017, 37(1):97-107. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201701009
[29] 汪品先, 章纪军, 赵泉鸿, 等.东海底质中的有孔虫与介形虫[M].北京:海洋出版社, 1988.
WANG Pinxian, ZHANG Jijun, ZHAO Quanhong, et al. Foraminiferal and Ostracoderm in Sediments in the East China Sea[M]. Beijing:China Ocean Press, 1988.
[30] 汪品先, 闵秋宝, 卞云华.南黄海西北部底质中有孔虫, 介形虫分布规律及其地质意义[C]//海洋微体古生物论文集.北京: 海洋出版社, 1980: 84-100.
WANG Pinxian, MIN Qiubao, BIAN Yunhua. A preliminary study of foraminiferal and ostracod assemblages of the Yellow Sea[C]//Papers on Marine Micropaleontology. Beijing: China Ocean Press, 1980: 84-100.
[31] 张静, 林景星, 剧远景, 等.东海E1孔晚更新世以来的地层、生物与环境[J].地质学报, 2004, 78(1):9-16. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200401002
ZHANG Jing, LIN Jingxing, JU Yuanjing, et al. Stratigraphy, biology and environment of the E1 core from the east China sea in late Pleistocene[J]. Acta Geologica Sinica, 2004, 78(1):9-16. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200401002
[32] 李小艳, 翦知湣, 石学法, 等.全新世东海内陆架泥质区有孔虫特征及其古环境意义[J].海洋地质与第四纪地质, 2012, 32(4):61-71. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=992a94cb-f04e-46a4-b73d-77f810ed1482
LI Xiaoyan, JIAN Zhinmin, SHI Xuefa, et al. Holocene foraminifera from the mud area of the inner shelf, east China sea and their paleoenvironmental significances[J]. Marine Geology & Quaternary Geology, 2012, 32(4):61-71. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=992a94cb-f04e-46a4-b73d-77f810ed1482
[33] 赵泉鸿, 翦知湣, 张在秀, 等.东海内陆架泥质沉积区全新世古环境变迁:有孔虫证据[J].海洋地质与第四纪地质, 2009, 29(2);79-86. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=e9b76966-00ed-42c0-a30c-319e8696ecb8
ZHAO Quanhong, JIAN Zhimin, ZHANG Zaixiu, et al. Holocene paleoenvironmental changes of the inner-shelf mud area of the east China sea: evidence from foraminiferal faunas[J]. Marine Geology & Quaternary Geology, 2009, 29(2):79-86. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=e9b76966-00ed-42c0-a30c-319e8696ecb8
[34] 邓兵, 李从先.长江三角洲地区第一古土壤层及其古气候记录[J].海洋地质与第四纪地质, 1999, 19(3):29-37. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=4cf35d7b-cc3e-4cab-be86-232c34de79a0
DENG Bing, LI Congxian. Paleoclimate recorded in the first layer of paleosoil in Yangtze delta area[J]. Marine Geology & Quaternary Geology, 1999, 19(3):29-37. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=4cf35d7b-cc3e-4cab-be86-232c34de79a0
[35] 陈报章, 李从先, 业治铮.长江三角洲北冀全新统底界和硬黏土层的讨论[J].海洋地质与第四纪地质, 1991, 11(2):37-46. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=9c1eae06-79df-4a49-aea4-145d9ca3eaf2
CHEN Baozhang, LI Congxian, YE Zhizheng. Holocene bottom boundary and hard clay band in the northern flank of the Changjiang river delta[J]. Marine Geology & Quaternary Geology, 1991, 11(2):37-46. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=9c1eae06-79df-4a49-aea4-145d9ca3eaf2
[36] 徐海.中国全新世气候变化研究进展[J].地球地球化学, 2001, 29(2):9-16. http://d.old.wanfangdata.com.cn/Periodical/dzdqhx200102002
XU Hai. Advance in researchon the Holocene climate fluctuations[J]. Geology-Geochemistry, 2001, 29(2):9-16. http://d.old.wanfangdata.com.cn/Periodical/dzdqhx200102002
[37] 王淑云, 吕厚远, 刘嘉麒.湖光岩玛珥湖高分辨率孢粉记录揭示的早全新世适宜期环境特征[J].科学通报, 2007, 52(11):1285-1291. http://d.old.wanfangdata.com.cn/Periodical/kxtb200711012
WANG Shuyun, LU Houyuan, LIU Jiaqi, et al. The Early Holocene optimum inferred from a high-resolution pollen record of Huguangyan Maar lake in Southern China[J]. Chinese Science Bulletin, 2007, 52(20):2829-2836. http://d.old.wanfangdata.com.cn/Periodical/kxtb200711012
[38] Berger A, Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Science Reviews, 1991, 10(4):297-317. doi: 10.1016/0277-3791(91)90033-Q
[39] Wang Y J, Chen H, Edwards R L, et al. Millennial and orbital-scale changes in the East Asian monsoon over the past 224, 000 years[J]. Nature, 2008, 451(28):1090-1093. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgjckx200902003
[40] Miller K G, Kominz M A, Browning J V, et al. The Phanerozoic record of global sea-level change[J]. Science, 2005, 310(5752):1293-1298. doi: 10.1126/science.1116412
[41] 类延斌, 张成君, 尚华明, 等.青藏高原东北部希门错湖岩心粒度特征及其环境意义[J].海洋地质与第四纪地质, 2006, 26(3):31-38. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=39c12edd-d087-45dd-b645-9f8450657b6b
LEI Yanbin, ZHANG Chengjun, SHANG Huaming, et al. The grain size characteristics of Ximencuo lake core in the northeast Tibet Plateau and its environmental significance[J]. Marine Geology & Quaternary Geology, 2006, 26(3):31-38. http://hydz.chinajournal.net.cn/WKD/WebPublication/paperDigest.aspx?paperID=39c12edd-d087-45dd-b645-9f8450657b6b
[42] Hori K, Saito Y, Zhao Q, et al. Evolution of the coastal depositional systems of the Changjiang (Yangtze) River in response to late Pleistocene-Holocene sea-level changes[J]. Journal of Sedimentary Research, 2002, 72(6):884-897. doi: 10.1306/052002720884
[43] Hori K, Saito Y, Zhao Q, et al. Progradation of the Changjiang River delta since the mid-Holocene[J]. Science in China Series B:Chemistry, 2001, 44(1):87-91. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=88181d57194a2a75776288c8f8191119
[44] Song B, Li Z, Saito Y, et al. Initiation of the Changjiang (Yangtze) delta and its response to the mid-Holocene sea level change[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 388:81-97. doi: 10.1016/j.palaeo.2013.07.026
[45] 李从先, 郭蓄明, 许志远, 等.全新世长江三角洲地区砂体的特征和分布[J].海洋学报, 1979, 1(2):252-268. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC197902006.htm
LI Congxian, GUO Xumin, XU Shiyuan, et al. The characteristics and distribution of Holocene sand bodies in Changjiang river delta area[J]. Acta Oceanologia sinica, 1979, 1(2):252-268. http://www.cnki.com.cn/Article/CJFDTOTAL-SEAC197902006.htm
[46] 王靖泰, 郭蓄民, 许世远, 等.全新世长江三角洲的发育[J].地质学报, 1981(1):69-83. http://d.old.wanfangdata.com.cn/Periodical/gdlxb200901012
WANG Jingtai, GUO Xumin, XU Shiyuan, et al. Evolution of the Holocene Changjiang Delta[J]. Acta Geologica Sinica, 1981(1):69-83. http://d.old.wanfangdata.com.cn/Periodical/gdlxb200901012
[47] 王中波, 杨守业, 张志珣, 等.东海陆架中北部沉积物粒度特征及其沉积环境[J].海洋与湖沼, 2012, 43(6):1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003
WANG Zhongbo, YANG Shouye, ZHANG Zhixun, et al. [Grain size characteristics of sediments and its depositional environment in the north of East China Sea[J]. Oceanologia et Limnologia Sinica, 2012, 43(6):1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003
[48] 刘红, 何青, 王元叶, 等.长江口表层沉积物粒度时空分布特征[J].沉积学报, 2007, 25(3):445-455. doi: 10.3969/j.issn.1000-0550.2007.03.017
LIU Hong, HE Qing, WANG Yuanye, et al. Temporal and spatial characteristics of surface sediment grain-size distribution in Changjiang estuary[J]. Acta Sedimentologica Sinica, 2007, 25(3):445-455. doi: 10.3969/j.issn.1000-0550.2007.03.017
[49] 同济大学海洋地质系三角洲科研组.全新世长江三角洲的形成和发育[J].科学通报, 1978, 23(5):310-313. http://cdmd.cnki.com.cn/Article/CDMD-10269-1015542986.htm
Delta Research Group of Department of Marine Geology, Tongji University. Formation and development of Yangtze Delta since the Holocene (in Chinese)[J]. Chinese Science Bulletin, 1978, 23(5):310-313. http://cdmd.cnki.com.cn/Article/CDMD-10269-1015542986.htm
[50] 王伟铭, 舒军武, 陈炜, 等.长江三角洲地区全新世环境变化与人类活动的影响[J].第四纪研究, 2010, 30(2):233-244. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201002001
WANG Weimin, SHU Junwu, CHEN Wei, et al. Holocene environmental changes and human impact in the Yangtze River Delta area, East China[J]. Quaternary Sciences, 2010, 30(2):233-244. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201002001
[51] Marcott S A, Shakun J D, Clark P U, et al. A reconstruction of regional and global temperature for the past 11300 years[J]. Science, 2013, 339(6124):1198-1201. doi: 10.1126/science.1228026
[52] 彭安玉.论明清时期苏北里下河自然环境的变迁[J].中国农史, 2006, 25(1):111-118. doi: 10.3969/j.issn.1000-4459.2006.01.016
PENG Anyu. On natural environment vicissitudes of Lixiahe Basin in North Jiangsu Province during Ming and Qing Dynasties[J]. Agricultural History of China, 2006, 25(1):111-118. doi: 10.3969/j.issn.1000-4459.2006.01.016
[53] 刘会远.黄河明清故道考察研究[M].南京:河海大学出版社, 1998:278.
LIU Huiyuan. Surveying of the Old Course of Yellow River in Ming-Qing Dynasties[M]. Nanjing: Hohai University Press, 1998:278.
-
图(5)
表(1)
计量
- 文章访问数: 2020
- PDF下载数: 44
- 施引文献: 0