渤海湾4.2ka事件初步研究
A preliminary study of the 4.2ka event along the coast of Bohai Bay
-
摘要: 相距3~20km的岭头、罾口河、俵口和空港物流中心4处埋藏牡蛎礁体的年代学研究证实,开始发育的时间不同,但同时在4.2~4.0ka cal BP时结束建礁,即其灭亡与“4.2ka事件”在时间上重合。岭头、罾口河剖面O稳定同位素和罾口河剖面孢粉数据进一步表明,4.5~4.3ka cal BP时研究区气候出现变冷变干的趋势,4.3~4.2ka cal BP逐渐好转,推测这一气候波动变化过程可能是对“4.2ka事件”的响应。Abstract: AMS 14C dating revealed that initiation timing of the four buried oyster reefs, Lingtou, Zengkouhe, Biaokou and Airport Logistic Center, 3~20km apart from each other, was different but the reef building-up at the four sites were almost simultaneously finished by accumulation of the thick muddy sediments at 4.2~4.0ka cal BP or so, which coincided with the ‘4.2ka event’. Furthermore, oxygen isotope study of the endogenic carbonate mud taken from the interior of the articulated oyster shells and the overlying muddy sediments in Zengkouhe and Lingtou profiles and pollen analysis from the same sampling positions were carried out. Both results indicate that the local climate condition tended to be cold and dry during the period of 4.5~4.3ka cal BP and then began to ameliorate in 4.3~4.2ka cal BP. The authors hold that this climate fluctuation was probably a response to the ‘4.2ka event’ in the study area.
-
Key words:
- Bohai Bay /
- oyster reef /
- 4.2ka event
-
-
[1] 刘浴辉, 孙霞, 郭彩青. 中国全新世4.2ka BP气候事件及其对古文明的影响[J]. 地质科技情报, 2013, 32(1):99-106.
[2] Wess H, Courty M A, Wetterstrom W, et al. The genesis and col-lapse of third millennium North Mesopotamian civilization[J]. Sci-ence, 1993, 261:995-1004.
[3] 许靖华. 太阳、气候、饥荒与民族大迁移[J]. 中国科学(D辑), 1998, 28(4):366-384.
[4] Cullen H M, deMenocal P B, Hemming S, et al. Climate change and the collapse of the Akkadian Empire:Evidence from the deep sea[J]. Geology, 2000, 288:379-382.
[5] Perry C A, Hus K J. Geophysical, archeological, and historical evi-dence support a solar-output model for cliamte change[J]. Proceed-ing of the National Academy of Sciences of the Unite States of America, 2000, 97(23):12433-12438.
[6] 方修琦, 连鹏灵. 岱海地区原始农业文化的衰落与环境演变的关系[J]. 地理研究, 2001, 20(5):623-627.
[7] An C B, Tang L Y, Barton L, et al. Climate change and cultural re-sponse around 4000 cal yr B. P. in the western part of Chinese Loess Plateau[J]. Quaternary Research, 2005, 63:347-352.
[8] 殷志强, 秦小光. 末次冰期以来松嫩盆地东部榆树年黄土堆积及其环境意义[J]. 中国地质, 2010, 37(1):212-222.
[9] 靳桂云, 刘东生. 华北北部中全新世降温气候事件与古文化变迁[J]. 科学通报, 2001, 46(20):1725-1730.
[10] Xu H, Hong Y T, Lin Q H, et al. Temperature variations in the past 6000 years inferred from d18O of peat cellulose from Hongyu-an, China[J]. Chinese Science Bulletin, 2002, 47(18):1578-1584.
[11] Hong Y T, Hong B, Lin Q H, et al. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene[J]. Earth and Planetary Science Letter, 2003, 211:371-380.
[12] Jiang W Y, Leroy S A G, Ogle N, et al. Natural and anthropogenic forest fires recorded in the Holocene pollen record from a Jinchuan peat bog, northern China[J]. Palaeogeography, Plaeoclimatology, Palaeoecology, 2008, 261:47-57.
[13] Hong Y T, Hong B, Lin Q H, et al. Synchronous climate anoma-lies in the western North Pacific and North Atlantic regions during the last 14000 years[J]. Quaternary Science Reviews, 2009, 28:840-849.
[14] Wang H, Hong Y T, Lin Q H, et al. Response of humification de-gree to monsoon climate during the Holocene from Hongyuan peat bog, eastern Tibetan Plateau[J]. Palaeogeography, Palaeoclima-tology, Palaeoecology, 2010, 286:171-177.
[15] Gasse F, Fontes J Ch, Campo Van E, et al. Holocene environmen-tal changes in Bangong Co Basin(Western Tibet). Part 4:Discus-sion and Conclusion[J]. Palaeogeography, Plaeoclimatology, Palaeo-ecology, 1996, 120:79-92.
[16] 张振克, 吴瑞金, 王苏民, 等. 全新世大暖期云南洱海环境演化的湖泊沉积记录[J]. 海洋与湖沼, 2000, 31(2):211-214.
[17] 白雁, 刘春莲, 郑卓, 等. 海南岛双池玛珥湖沉积中的碳、氮地球化学记录及其古环境意义[J]. 古地理学报, 2003, 5(1):87-93.
[18] 刘兴起, 沈吉, 王苏民, 等. 16ka以来青海湖湖湘自生碳酸盐沉积记录的古气候[J]. 高校地质学报, 2003, 9(1):38-46.
[19] Peng Y J, Xiao J L, Nakamurab T, et al. Holocene East Asian mon-soonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China[J]. Earth and Planetary Science Letters, 2005, 23(1/2):467-479.
[20] 申洪源, 贾玉连, 李徐生, 等. 内蒙古黄旗海不同粒级湖泊沉积物Rb、Sr组成与环境变化[J]. 地理学报, 2006, 61(11):1208-1217.
[21] 黄昌庆, 冯兆东, 马玉贞, 等. 巴汉淖孢粉记录的全新世环境变化[J]. 兰州大学学报(自然科学版), 2009, 45(4):7-12.
[22] 李延勇, 李红春, 袁道先, 等. 重庆新崖洞XY6石笋4.5ka以来高分辨率δ18O、δ13C记录的气候变化[J]. 中国岩溶, 2006, 25(2):95-100.
[23] 张美良, 林玉石, 朱晓燕, 等. 云南宁蒗地区中全新世晚期气候变化的石笋记录[J]. 海洋地质与第四纪地质, 2006, 26(1):35-40.
[24] Yi S, Saito Y, Zhao Q H, et al. Vegetation and climate changes in the Changjiang(Yangtze River) Delta, China, during the past 13000 years inferred from pollen records[J]. Quaternary Science Reviews, 2003, 22:1501-1519.
[25] Helge W A, Frank L, Jürgen P. A pronounced dry event recorded around 4.2ka in brine sediments from the northern Rea Sea[J]. Quaternary Research, 2006, 66:432-441.
[26] 黄光庆. 珠江三角洲新石器考古文化与古地理环境[J]. 地理学报, 1996, 51(6):508-517.
[27] 王宏, 范昌福, 李建芬, 等. 渤海湾西北岸牡蛎礁研究概述[J]. 地质通报, 2006, 25(3):315-331.
[28] 王海峰, 王宏, 范昌福, 等. 天津空港牡蛎礁:中全新世环境恶化与新构造控礁作用[J]. 地质通报, 2012, 31(9):1387-1393.
[29] Stuiver M, Braziunas T. Modelling atmospheric 14C influences and 14C ages of marine samples to 10000 BC[J]. Radiocarbon, 1993, 35:137-189.
[30] Reimer P J, Bard E, Bayliss A, et al. IntCal13 and MARINE13 ra-diocarbon age calibration curves 0-50000 years cal BP[J]. Radiocar-bon, 2013, 55(4):1869-1887.
[31] Southon J, Kashgarian M, Fontugne M, et al. Marine reservoir cor-rections for the Indian Ocean and Southeast Asia[J]. Radiocarbon, 2002, 44:167-180.
[32] Anderson L, Finney B P, Shapley M D. Lake carbonate-δ18O re-cords from the Yukon Territory, Canada:Little Ice Age moisture variability and patterns[J]. Quaternary Science Reviews, 2011, 30:887-898.
[33] 李春园, 孙蕾, 葛璇, 等. 南海北部表层沉积物碳酸盐含量和δ18O及δ13C的空间分布与粒径分布特征及其控制因素[J]. 海洋学报, 2013, 35(3):246-254.
[34] 王爱军, 汪亚平. 江苏王港潮间带表层碳酸盐的沉积特征[J]. 江苏地质, 2004, 28(2):90-95.
[35] 王绍武. 全新世气候变化[M]. 北京:气象出版社, 2011:283.
[36] Masson-Delmotte V, Schultz M, Abe-Ouchi A, et al. Information from Paleoclimate Archives[C]//Climate Change 2013, The Physi-cal Science Basis, Contribution of Working Group I to the Fifth As-sessment Report of the Intergovernmental Panel of Climate Change. Cambridge University Press, Cambridge, United King-dom and New York, NY, USA, 2013:383-464.
[37] Bond G C, Showers W, Cheseby M, et al. A Pervasive millennialscale cycle in North Atlantic Holocene and glacial climates[J]. Sci-ence, 1997, 278:1257-1266.
[38] Mayewski P A, Rohling E E, Stager J C, et al. Holocene climate variability[J]. Quaternary Research, 2004, 62:243-255.
[39] 王绍武. 全新世气候[J]. 气候变化研究进展, 2009, 5(4):247-248.
-
计量
- 文章访问数: 1159
- PDF下载数: 60
- 施引文献: 0