唐朝末年以来广西柳州干湿变化及人类活动演变

doi:10.13284/j.cnki.rddl.003064

摘要/Abstract

摘要： 中世纪暖期和小冰期是近2 000年气候变化中重要的气候事件，厘清其在低纬度地区干湿变化特征及其对古代农业发展及人口增长的影响，具有重要的意义。通过对广西柳州岩溶洞穴中一60 cm岩芯进行孢粉、炭屑分析发现，研究区的气候、稻作农业从唐末以来先后经历了6个阶段演化：1）875―940 a A.D.，C/P值及花粉记录指示：研究区气候整体偏干，水稻种植减少；2）940―1 050 a A.D.，C/P值及花粉记录指示：夏季风增强，水稻种植稍增长，人口增加；3）1 050―1 140 a A.D.，C/P值及花粉记录指示：夏季风减弱，稻作农业及人口较前期有所增长；4）1 140―1370 a A.D.，C/P值及莎草科花粉含量指示：研究区当时气候处于“中世纪暖期”温暖湿润期，稻作农业面积扩大，人口增加；5）1 370―1 900 a A.D.，C/P值及莎草科花粉含量指示：“小冰期”气候变干，水稻种植及人口逐渐减少；6）1 900―2 009 a A.D.气候变暖湿，水稻种植扩大，人口迅速增长。进一步对研究区气候事件与稻作农业及人口关系研究发现：历史时期气候事件与水稻种植、人口具有耦合关系，即中世纪暖期，气候暖湿，水稻种植扩大，人口增殖；小冰期，气候冷干，水稻种植萎缩，人口锐减。在非原地沉积时，莎草科和C/P 对水分反映敏感，可以用来指示气候干湿变化。

关键词: 孢粉, 炭屑, 人类活动, 干湿变化, 中世纪暖期, 小冰期, 广西柳州

Abstract: Medieval Warm Period and Little Ice Age are important climatic events in the last two millenniums. To clarify the characteristics of dry and wet changes in low latitudes and its influence on the development of ancient agriculture and population growth is of great significance. A 60cm continuous cave-sedimental core from Liuzhou, Guangxi province, Southwest China, based on palynological investigation, has revealed that since the 875a A.D., climate and human activities of the research area has undergone six stages：875a A.D.- 940a A.D.， the pollen and C/P index both indicated drought event，meanwhile the rice cultivation gradually dropped. The population of the research region was poorly recorded after Late Tang Dynasty. 940a A.D.-1050a A.D., with the climate gradually transferring to humid，the rice cultivation generally developed, and so did the population. 1050a A.D.-1140a A.D., the C/P index pollen record and the stalagmite δ18O all referred this stage as a relatively dry climate, while the rice cultivation and population was similar with prior stage. 1140a A.D.-1370a A.D., Medieval Warm Period, the C/P and Cyperaceae pollen percentage was high, and the high rice pollen and low arboreal pollen also revealed strengthened human disturbance. The historical record indicated that the population of the research area grew quickly in this period. 1370a A.D.-1900a A.D.，Little Ice Age, the climate was drying and cooling， indicated by pollen analysis, which affected the rice cultivation, and the population reduced continuously. 1900a A.D.-2009a A.D. the climate recovered and the rice cultivation area expanded. The result also shows that the climate extremes have a strong corresponds with rice-cultivating and population：during Medieval Warm Period, climate was warm and humid which contributed to the growth of rice-cultivating and population, while in LIA, cold and dry climate decreased the population and the area of rice cultivation. When the Cyperaceae pollen is not local deposit, Cyperaceae pollen percentage and C/P, which are sensitive to moisture, can be used to indicate dry and wet climate changes.

Key words: pollen, charcoal, human activity, dry-humid fluctuation, Medieval Warm Period, Little Ice Age, Liuzhou Guangxi

赵增友，石胜强，殷建军，张春生，代稳，秦趣. 唐朝末年以来广西柳州干湿变化及人类活动演变[J]. 热带地理, 2018, 38(4): 575-585.

ZHAO Zengyou，SHI Shengqiang，YIN Jianjun，ZHANG Chunsheng，DAI Wen，QIN Qu. Climate and Human Disturbance Changes since the Late Tang Dynasty in the Karst Area of Liuzhou，Guangxi[J]. TROPICAL GEOGRAPHY, 2018, 38(4): 575-585.

参考文献

BENJAMIN C E，HORTON B P and STANLEY J D．2011．Nile delta vegetation response to Holocene climate variability．Geology，40：615- 618．

COSFORD J，QING H，EGLINGTON B，MATTEY D，YUAN D X, ZHANG M L and CHENG H．2008．East Asian monsoon variability since the Mid-Holocene recorded in a high-resolution，absolute-dated aragonite speleothem from eastern China．Earth and Planetary Science Letters，275：296-307．

蔡演军，彭子成，BECK W，张兆峰．2005．洞穴次生碳酸盐中“死碳”对14C法测年的影响．科学通报，50（5）：459-463．[CAI Yanjun，PENG Zicheng，BECK W and ZHANG Zhaofeng．2005．The effect of dead A.D. carbon in cave secondary carbonates on dating by 14C method．Chin. Sci. Bull.，50（5）：459-463．]

陈豆．2015．天山大龙池与柴达木盆地巧海过去2000年沉积记录．兰州：兰州大学．[CHEN Dou．2015．The sediment record of lake Dalongchi and lake Gahai for the past 2000 years．Lanzhou：Lanzhou University．]

FEAGRI K，IVERSEN J．1989．Textbook of Pollen Analysis．Oxford：Blackwell．

GILLSON L．2006．A “large infrequent disturbance” in an East African savanna．Afr. J. Ecol.，44：458-467．

GRIMM E C，2004．TGview．Version 2.0.2．Springfield：Illinois State Museum Research Collection Center．

葛剑雄，吴松弟，曹树基，冻国栋，侯杨方．2000．中国人口史．上海：复旦大学出版社．[GE Jianxiong，WU Songdi，CAO Shuji，DONG Guodong and HOU Yangfang．2000．History of Chinese population．
Shanghai：Fudan University Press．]

葛全胜，刘浩龙，郑景云，萧凌波．2013．中国过去2000年气候变化与社会发展．自然杂志，35（1）：9-21．[GE Quansheng，LIU Haolong，ZHENG Jingyun and XIAO Lingbo．2013．The Climate change and social development over the last two millennia in China．Chin. J .of Nat.，35（1）：9-21．]

葛全胜，郑景云，郝志新，张学珍，方修琦，王欢，闫军辉．2014．过去2000年中国气候变化研究的新进展．地理学报，69（9）：1248- 1258．[GE Quansheng，ZHENG Jingyun，HAO Zhixin，ZHANG Xuezhen，FANG Xiuqi，WANG Huan and YAN Junhui．2014．State-of- the-arts in the study of climate changes over China for the past 2000 years．Acta Geographica Sinica，69（9）：1248-1258．]

广西壮族自治区地方志编纂委员会．1993．广西通志·人口志．南宁：广西人民出版社．[Guangxi editorial committee of local chronicles， 1993．Guangxi chronicle·Population chronicle．Nanling：Guangxi People’s Press．]

郭文佳．2009．论宋代劝课农桑兴修水利的举措．考古研究，（3）：25- 27．[GUO Wenjia．2009．Song Dynasty attaching importance to Agriculture Water Conservancy Measures．Archaeological Research，（3）：25-27．]

HECKENBERGER M J，KUIKURO A，KUIKURO U T，RUSSELLET J C, SCHMIDT M，FAUSTO C and FRANCHETTO B．2003．Amazonia 1492：Pristine Forest or Cultural Parkland?．Sci，301：1710-1714．

韩爱艳，曾砺锋，黄康有，廖文波，郑卓，陈聪．2016．罗霄山脉山地沼泽全新世以来的古气候记录．热带地理，36（3）：477-485，520．[HAN Aiyan，ZENG Lifeng，HUANG Kangyou，LIAO Wenbo，ZHEN Zhuo and CHEN Cong．2016．Holocene Climate Records from a Mountain Wetland in Luoxiao Ranges．Tropical Geography，36（3）：477-485，520．]

侯光良，魏海成，鄂崇毅，孙永娟．2013．青藏高原东北缘全新世人类活动与环境变化——以青海湖江西沟2号遗迹为例．地理学报，68（3）：380-388．[HOU Guangliang，Wei Haicheng，E Chongyi and SUN Yingjuan．2013．Human activities and environmental change in Holocene in the northeastern margin of Qinghai-Tibet Plateau：A case study of JXG2 relic site in Qinghai Lake．Acta Geographica Sinica，68（3）：380-388．]

黄康有，何嘉卉，宗永强，郑卓，章桂芳，曹玲珑．2016．珠江三角洲三水盆地早全新世以来孢粉分析与古环境重建．热带地理，36（3）：364-373．[HUANG Kangyou，HE Jiahui，ZONG Yingqiang，ZHEN Zhuo，ZHANG Guifang and CAO Linglong．2016．Holocene Paleoenvironment Reconstruction Based on Pollen Data in the Sanshui Basin，Northern Pearl River Delta．Tropical Geography，36（3）：364-373．]

IPCC．2007．Climate Change 2007-The Physical Science Basis．New York：Cambridge University Press．

LI Jinyun，LI Hongchun，LI Tingyong，MII H S，YU T L，SHEN Chuanchou and XU Xiaomei．2017．High-resolution d18O and d13C records of an AMS 14C and 230Th/U dated stalagmite from Xinya Cave in Chongqing：Climate and vegetation change during the late Holocene．Quat．Int，http：//dx.doi.org/10.1016/j.quaint.2017.06.075.

LOZHKIN A V，ANDERSON P M，VARTANYAN S L，BROWN T A，BELAYA B V and KOTOV A N．2001．Late quaternary paleoenvironments and modern pollen data from Wrangel Island（Northern Chukotka）．Quat．Sci．Rev，20：217-233．

李偏，张茂恒，孔兴功，张春霞，汪永进，赵侃．2010．近2000年来东亚夏季风石笋记录及与历史变迁的关系．海洋地质与第四纪地质，30（4）：201-208．[LI Pan，ZHANG Maoheng，KONG Xinggong，ZHANG Chunxia，WANG Yongjin and ZHAO Kan．2010．A stalagmite-record of East Asian summer monsoon in the last 2000 years and its correlation with historical records．Mari．Geo and Quat．Geo，30（4）：201-208．]

李文静．2014．腾冲青海湖泊沉积记录的近2000年以来的气候环境演化[D]．昆明：云南师范大学．[LI Wenjing．2014．Climate and environment variation recorded in the sediment of Qinghai lake in Tengchong since 2000 a BP[D]．Kunming：Yunnan Normal University．]

李宜垠，侯树芳，莫多闻．2009．湖北屈家岭遗址孢粉、炭屑记录与古文明发展．古地理学报，11（6）：702-710．[LI Yiyin，HOU Shufang and MO Duowen．2009．Records for pollen and charcoal from Qujialing archaeological site of Hubei and ancient civilization development．J．of Pala，11（6）：702-710．]

满美玲，郑卓，李杰，王梦瑗．2016．广西北部山地沼泽20 ka以来的碳同位素组成与气候变化．热带地理，36（3）：468-476．[MAN Meiling，ZHENG Zhuo，LI Jie and WANG Mengyuan．2016．Carbon Isotope Compositions and Climate Changes of the Past 20,000Years Inferred from a Mountainous Peat Bog of Northern Guangxi．Tropical Geography，36（3）：468-476．]

欧祖兰，苏宗明，李先琨．2004．广西岩溶植被植物区系．广西植物，24（4）：302-310．[OU Zulan，SU Zongming and LI Xiankun．2004．
Flora of Karst vegetation in Guangxi．Guihaia，24（4）：302-310．]

PEDERSON D C，PETEET D M，KURDYLA D and GUILDERSON T．2005．Medieval Warming，Little Ice Age，and European impact on the environment during the last millennium in the lower Hudson Valley，New York，USA．Quat．Res.，63：238-249．

覃嘉铭，林玉石，张美良，李红春．2000a．桂林全新世石笋高分辨率δ13C记录及其古生态意义．第四纪研究，20（4）：351–358．[QIN Jiaming，LIN Yushi，ZHANG Meiliang and LI Hongcun．2000．High resolution records of δ13C and their paleoecological significance from stalagmites formed in Holocene epoch in Guilin．Quat. Sci.，20（4）：351–358．]

覃嘉铭，袁道先，林玉石，张美良，李彬．2000b．桂林44 ka BP石笋同位素记录及其环境解译．地球学报，21（4）：407-416．[QIN Jiaming，YUAN Daoxian，LIN Yushi，ZHANG Meiliang and LI Bin．2000．
Isotopic records of stalagmites from Guilin since 44 ka BP and their environmental interpretation．Acta Geo．Sin.，21（4）：407–416．]

覃军干，张新荣，张强，周建超．2016．近1000年以来气候波动在广西桂北地区沉积物中的记录．第四纪研究，36（2）：268-277．[QIN Jungan，ZHANG Xinrong，ZHANG Qiang，ZHOU Jianchao．2016．
Climate oscillations recorded in the sediment from North Guilin，Guangxi during the past 1000yeaes．Quat．Sci，36（2）：268-277．]

SINGH G．1971．The Indus Valley culture seen in the context of postglacial climatic and ecological studies in northwest India．Archaeology and Physical Anthropology in Oceania，6：177-189．

SWAINA M，KUTZBACH J E and HASTENRATH S．1983．Estimates of Holocene precipitation for Rajasthan，India，based on pollen and lake-level data．Quat．Res，19：1-17．

舒军武，王伟铭，陈伟．2007．太湖平原细部全新世以来植被与环境变化．微体古生物学报，24（2）：210-221．[SHU Junwu，WANG Weiming and CHEN Wei．2007．Holocene vegetation and environment changes in the NW Taihu Plain，Jiangsu Pronince，East China．Acta Micro palae．Sin.，24（2）：210-221．]

TANG Lingyu，SHEN Caiming，LI Chunhai，PENG Jinlan，LIU Hui，LIU Kanbiu，MORRILL C，OVERPECK J T，COLE J E and YANG Bao．2009．Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200yr BP．Science in China Series D：Earth Science，52（8）：1104-1114．

TED M，MICHAEL C M and JOHN S P．2002．Encyclopedia of global environment change．Chichester：John Wiley＆Son，Ltd.
．
WANG Yongjin，CHENG Hai，EDWARDS R L，HE Yaoqi，KONG Xinggong，AN Zhisheng，WU Jiangying，KELLY M J，DYKOSKI C A and LI Xiangdong．005．The Holocene Asian monsoon：links to solar changes and North Atlantic climate．Sci.，308：854–857．

魏柱灯，方修琦，苏筠，萧凌波．2014．过去2000年气候变化对中国经济与社会发展影响研究综述．地球科学进展，29（3）：336-343．[WEI Zhudeng，FANG Xiuqi，SU Yun and XIAO Lingbo．2014．A review of climatic impacts on Chinese socio-economic development over the past 2000 years．AdA. D. v. in. Ear. Sci，29（3）：336-343．]

许清海，曹现勇，王学丽，李月丛，荆志淳，唐际根．2010．殷墟文化发生的环境背景及人类活动的影响．第四纪研究，30（2）：273- 286．[XU Qinghai，CAO Xianyong，WANG Xueli，LI Yuecong，JING Zhichun and TANG Jigen．2010．Generation of Yinxu culture：Environmental background and impacts of human activities．Quat. Sci.，30（2）：273-286．]

YANCHEVA G，NOWACZYK N R，MINGRAM J，DULSKI P，SCHETTLER G，NEGENDANK J F W，LIU J Q，SIGMAN D M，PETERSON L C and HAUG G H．2007．Influence of the intertropical convergence zone on the East-Asian monsoon．Nat.，445：74-77．

YANG Bao，QIN Chun，WANG Jianglin，HE Minghui，MELVIN T M，OSBORN T J and BRIFFA K R．2014．A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau．PNAS，111（8）：2903-2908．

YANG Yiping，ZHANG Hucai，CHANG Fengqin，MENG Hongwei，PAN Anding，ZHEN Zhuo and XIANG Rong．2016．Vegetation and climate history inferred from a Qinghai Crater Lake pollen record from Tengchong，southwestern China．Palae，http://dx.doi.org/10.1016/j. palaeo.2016.07.017．

YIN Jianjun，LI Hongchun，RAO Zhiguo，SHEN Chuanchou，MII H S，PILLUTLA R K，HU Hsunming，LI Yunxia and FENG Xiahong．2017．
Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain，North China reflected by stalagmite d18O and d13C records from Zhenzhu Cave．Quat．Int，47 ：89-101．

YIN Jianjun，YUAN Daoxian，LI Hongchun，CHENG Henyi，LI Tingyong，EDWARDS R L，LIN Yushi，QIN Jiaming，TANG Wei，ZHAO Zengyou and MII H S．2014．Variations in the Asian monsoon intensity and dry-wet condition since the Little Ice Age in central China revealed by an aragonite stalagmite．Clim．Past，10：1803-1816．

乐远福，郑卓，BARRY V R，黄博津，黄康有，CHEDDADI R．2016．闽江下游全新世孢粉记录的植被与环境变化．热带地理，36（3）：417-426．[YUE Yuanfu，ZHENG Zhuo，BARRY V R，HUANG Bojin，HUANG Kangyou and CHEDDADI R．2016．Vegetation and Environmental Changes Inferred from a Holocene Pollen Spectrum in the Lower Reaches of Min River．Tropical Geography，36（3）：417-426．]

杨士雄，郑卓，黄康有，李杰，韦潇君，许清海．2012．华南主要作物和果蔬类现代花粉形态及农业考古研究价值．微体古生物学报，29（1）：80-98．[YANG Shixiong，ZHENG Zhuo，HUANG Kangyou，LI Jie，WEI Xiaojun and XU Qinghai．2012．Pollen morphology of modern principal crops vegetables and fruits in south China and their value for agricultural archaeology．Acta Mic．pala．Sin，29（1）：80-98．]

姚檀栋，秦大河，徐柏青，杨梅学，段克勤，王宁练，王有清，侯书贵．2006．冰芯记录的过去1000a青藏高原温度变化．气候变化研究进展，2（3）：99-103．[YAO Tandong，QIN Dahe，XU Baiqing，YANG Meixue，DUAN Keqin，WANG Ninglian，WANG Youqing and HOU Shugui．2006．Temperature change over the Past Millennium recorded in ice cores from the Tibetan Plateau．AdA. D. v. Clim. Change. Res.，2（3）：99-103．]

ZHANG D D，ZHANG J，LEE H F and HE Yuanqing．2007．Climate Change and War Frequency in Eastern China over the Last Millennium．Hum. Ecol.，35：403–414．

ZHANG Pingzhong，CHENG Hai，EDWARDS R L，CHEN Fahu，WANG Yongjin，YANG Xunlin，LIU Jian，TAN Ming，WANG Xianfeng，LIU Jinghua，AN Chunlei，DAI Zhibao，ZHOU Jing，ZHANG Dezhong，JIA Jihong，JIN Liya and JOHNSON．2008．A test of climate，sun and culture relationships from an 1810-year Chinese cave record．Sci.，322：940-942．

ZHANG Deer，LI Hongchun，KU T L and LU Longhua．2010．On linking climate to Chinese dynastic change：Spatial and temporal variations of monsoonal rain．Chin. Sc.i Bull.，55：77?83．

ZHAO Kan，WANG Yongjin，EDWARDS R L，CHENG Hai，LIU Dianbing and KONG Xinggong．2015．A high-resolved record of the Asian Summer Monsoon from Dongge Cave，China for the past 1200 years．Qua. Sci. Rev，122：250-257．

ZHENG Jingyun，WANG Weichyung，GE Quansheng，MAN Zhimin and ZHANG P Y．2006．Precipitation variability and extreme events in Eastern China during the past 1500 years．Terr. Atmo.s Ocean. Sci.，17（3）：579-592．

张德二．2004．中国三千年气象记录总集．江苏：江苏教育出版社．[ZHANG De’er．2004．Chinese three thousand years meteorological record collection．Jiangsu：Jiangsu Education Press．]
张美良，袁道先，林玉石，覃嘉铭，章程，程海．2003．桂林响水洞6.00ka BP以来石笋高分辨率的气候记录．地球学报，24（5）：439–444．[ZHANG Meiliang，YUAN Daoxian，LIN Yushi，QIN Jiaming，ZHANG Cheng and CHENG Hai．2003．High resolution climatic records of stalagmite from Xiangshui Cave in Guilin since 6.00 ka BP．Acta Geosci. Sin.，24（5）：439–444．]

郑景云，郝志新，张学珍，刘浩龙，李明启，葛全胜．2014．中国东部过去2 000年百年冷暖的旱涝格局．科学通报，59（30）：2964- 2971．DOI：10.1360/N972014-00393．[ZHENG Jingyun，HAO Zhixin，ZHANG Xuezhen，LIU Haolong，LI Mingqi and GE Quansheng．2014．Drought/flood spatial patterns in centennial cold and warm periods of the past 2000 years over eastern China．Chin. Sci. Bull.（Chin. Ver.），59（30）：2964–2971．DOI：10.1360/N972014- 00393．]

郑景云，邵雪梅，郝志新，葛全胜．2010．过去2000年中国气候变化研究．地理研究，29（9）：1561-1570．[ZHENG Jingyun，SHAO Xuemei，HAO Zhixin and GE Quansheng．2010．An overview of research on climate change in China during the past 2000 years．Geo. Res.，29（9）：1561-1570．]

郑维宽．2005．近六百年来广西气候变化研究．社会科学战线，（6）：155-160．[ZHENG Weikuan．2005．The last 600 years climate change of Guangxi．Soci. Sci. Front，（6）：155-160．]

郑维宽．2009．历史时期广西旱稻的种植变迁．农业考古，（1）：60- 73．[ZHENG Weikuan．2009．Change of planting of upland rice in Guangxi history．Agri. Arch.，（1）：60-73．]

中国湿地植被编辑委员会．1999．《中国湿地植被》．北京：科学出版社．[Wetland Vegetation Editorial Committee of China．1999．Wetland Vegetation in China．Beijing：Science Press．]

周建超，覃军干，张强，张春来，蒋仕清．2015．广西桂林岩溶区中全新世以来的植被、气候及沉积环境变化．科学通报，60（13）：1197-1206．[ZHOU Jianchao，QIN Jungan，ZHANG Qiang，ZHANG Chunlai and JIANG Shiqing．2015．Vegetation，climate and depositional environment changes since the middle Holocene in the karst area of Guilin，Guangxi．Chin. Sci. Bull.，60（13）：1197–1206．]

[1]	侯光良，许长军，兰措卓玛，朱燕. 末次冰盛期中国人类活动的响应与适应[J]. 热带地理, 2018, 38(6): 819-827.
[2]	李扬，余克服，王英辉，郭靖，黄学勇，裴继影，罗燕秋. 三亚鹿回头岸礁海域夏季表层海水营养盐年际变化特征[J]. 热带地理, 2017, 37(5): 708-717.
[3]	黄康有，何嘉卉，宗永强，郑卓，章桂芳，曹玲珑．. 珠江三角洲三水盆地早全新世以来孢粉分析与古环境重建 [J]. 热带地理, 2016, 36(3): 364-373.
[4]	余少华，陈芳，谢叶彩，周洋，吴聪，陈炽新，龙桂．. 珠江口万顷沙晚第四纪沉积及古环境重建[J]. 热带地理, 2016, 36(3): 374-387.
[5]	乐远福，郑卓，Barry V ROLETT，黄博津，黄康有，Rachid CHEDDADI．. 闽江下游全新世孢粉记录的植被与环境变化[J]. 热带地理, 2016, 36(3): 417-426.
[6]	马婷，郑卓，满美玲，李杰，彭环环，韩爱艳，黄康有．. 南亚热带全新世火灾记录的气候变化及人类影响[J]. 热带地理, 2016, 36(3): 486-494.
[7]	邓晓宇，张强，孙鹏，方朝阳. 气候变化和人类活动对信江流域径流影响模拟[J]. 热带地理, 2014, 34(3): 293-301.
[8]	王丽荣，余克服，赵焕庭，张乔民. 南海珊瑚礁经济价值评估[J]. 热带地理, 2014, 34(1): 44-49.
[9]	杨士雄, 郑卓, 谭惠忠, 张镇洪, 王宏, 李杰. 香港西贡壕涌新石器以来的环境演变及人类活动[J]. 热带地理, 2011, 31(4): 339-345.
[10]	郑文武, 邹君, 田亚平, 邓运员. 基于RS和GIS的区域人类活动强度空间模拟[J]. 热带地理, 2011, 31(1): 77-81.
[11]	施祺, 赵美霞, 黄玲英, 严宏强, 张会领. 三亚鹿回头岸礁区人类活动及其对珊瑚礁的影响[J]. 热带地理, 2010, 30(5): 486-490,509.
[12]	李猷, 王仰麟, 彭建, 刘珍环, 吴健生. 快速城市化地区海岸线分维动态演变研究——以深圳市为例[J]. 热带地理, 2009, 29(5): 429-433.
[13]	田光进. 全球化与全球变化关系研究[J]. 热带地理, 2009, 29(2): 150-155.
[14]	潘安定, 陈碧姗, 刘会平, 杨木壮, 王志英. 孢粉学定量重建古气候方法探讨[J]. 热带地理, 2008, 28(6): 493-497.
[15]	肖清华, 朱创鑫. 1400-1950年广东冻灾特征[J]. 热带地理, 2008, 28(6): 508-512.