The hydroclimate changes in the northern Okinawa Trough during middle Holocene: Evidence from planktonic foraminiferal assemblages

XU Ye; CHANG Fengming; LI Tiegang; ZHAO Song; CUI Yikun

doi:10.16562/j.cnki.0256-1492.2017122101

Marine Geology & Quaternary Geology > 2019 > 39(1): 113-123. > DOI: 10.16562/j.cnki.0256-1492.2017122101

XU Ye, CHANG Fengming, LI Tiegang, ZHAO Song, CUI Yikun. The hydroclimate changes in the northern Okinawa Trough during middle Holocene: Evidence from planktonic foraminiferal assemblages[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 113-123. DOI: 10.16562/j.cnki.0256-1492.2017122101

Citation:

PDF (2748 KB)

The hydroclimate changes in the northern Okinawa Trough during middle Holocene: Evidence from planktonic foraminiferal assemblages

XU Ye^1,2,,
CHANG Fengming^1,3,
LI Tiegang^1,4,
ZHAO Song^1,2,
CUI Yikun^1,2

1.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Science, Qingdao 266071, China
2.
University of Chinese Academy of Science, Beijing 100049, China
3.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
4.
Key Laboratory of Marine Sedimentology and Environment Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China

More Information

Received Date: December 20, 2017
Revised Date: April 20, 2018

Graphical Abstract

Abstract

Abstract

Planktonic foraminifera assemblages in the northern East China Sea are significantly influenceed by both the Changjiang Diluted Water and Kuroshio Current. A total of 28 species in the coaser faction (>150μm) are identified based on planktic foraminifera analysis of 178 samples from core NOKT-3 in the northern Okinawa Trough. The results show that variations in percentage of Globigerina quinqueloba is characterized by sharp fluctuation in early Mid-Holocene and gradual decline in late Mid-Holocene. This low temperature and low salt salinity species is an indicator of the Changjiang Diluted Water, which is controlled by the East Asian summer monsoon precipitation. Therefore, the evolution of precipetation in the middle and lower reaches of the Yangtze River between 6330 and 3890aBP can be divided into three major stages based on variations in its content: (1) high precipetation during the period of 6330~4950aBP, which correspondes to the Holocene optimum; (2) a decreased trend of precipetation from 4950 to 4600aBP, implying termination of the Holocene optimum; (3) a marked decrease in the monsoon precipitation between 4600 and 3890aBP, indicating an arid climate condition. This precipetation pattern could be related to the general weakening and southeastward retreat of the East Asian summer monsoon resulted from the decreased solar-radiation in the northern hemisphere during the Middle Holocene. Moreover, remarkably high abundance of P. obliquiloculat during 6330~5100aBP, which is normally an indicator species of the Kuroshio Current, suggests that influence of the Kuroshio Current in the Okinawa Through was persistently strong. The abundance of P. obliquiloculata sharply decreased during 5100~4000aBP, well corresponding to the so-called Pulleniatina minimum event (PME). Our results show that there were not a cold climate condition corresponding to the PME during the period of late Mid-Holocene. In addition, enhancement of the El Niño-like condition in the tropical Pacific region during this time window also can not fully explain the occurrence of PME in the northern Okinawa Trough.
- East Asian summer monsoon,
- Changjiang Diluted Water,
- Kuroshio Current,
- P. obliquiloculata Minimum Event,
- Middle Holocene

FullText(HTML)

References (46)

References

[1]	郑伟鹏, 俞永强.一个耦合气候系统模式模拟的中全新世时期亚洲季风系统变化[J].第四纪研究, 2009, 29(6): 1135-1145. doi: 10.3321/j.issn:1001-7410.2004.01.004 ZHENG Weipeng, YU Yongqiang. Simulations of East Asian climate at 6kaBP[J]. Quaternary Sciences, 2004, 24(1): 28-38. doi: 10.3321/j.issn:1001-7410.2004.01.004
[2]	Chen Z Y, Song B P, Wang Z H, et al. Late Quaternary evolution of the sub-aqueous Yangtze Delta, China: sedimentation, stratigraphy, palynology, and deformation[J]. Marine Geology, 2000, 162: 423-441. doi: 10.1016/S0025-3227(99)00064-X
[3]	Yi S, Saito Y, Zhao Q H, et al. Vegetation and climate changes in the Changjiang (Yangtze River) Delta, China, during the past 13, 000 years inferred from pollen records[J]. Quaternary Science Reviews, 2003, 22(14): 1501-1519. doi: 10.1016/S0277-3791(03)00080-5
[4]	Du Y, Cai S M, Zhang X Y, et al. Interpretation of the environmental change of Dongting Lake, middle reach of Yangtze River, China, by ²¹⁰Pb measurement and satellite image analysis[J]. Geomorphology, 2001, 41(2-3): 171-181. doi: 10.1016/S0169-555X(01)00114-3
[5]	Yu K F, Zhao J X, Wei G J, et al. Mid-late Holocene monsoon climate retrieved from seasonal Sr/Ca and δ¹⁸O records of Porites lutea corals at Leizhou Peninsula, northern coast of South China Sea[J]. Global and Planetary Change, 2005, 47(2-4): 301-316. doi: 10.1016/j.gloplacha.2004.10.018
[6]	Li B, Liu H, Wu L, et al. Linking the vicissitude of Neolithic cities with mid Holocene environment and climate changes in the middle Yangtze River, China[J]. Quaternary International, 2014, 321: 22-28. doi: 10.1016/j.quaint.2013.11.018
[7]	Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1-2): 71-86. doi: 10.1016/j.epsl.2005.01.036
[8]	Hu C Y, Henderson G M, Huang J H, et al. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records[J]. Earth and Planetary Science Letters, 2008, 266(3-4): 221-232. doi: 10.1016/j.epsl.2007.10.015
[9]	Dong J G, Wang Y J, Edwards R L, et al. A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China[J]. The Holocene, 2010, 20(2): 257-264. doi: 10.1177/0959683609350393
[10]	Chang Y P, Wang W L, Yokoyama Y, et al. Millennial-scale planktic foraminifer faunal variability in the East China Sea during the Past 40000 Years (IMAGES MD012404 from the Okinawa Trough)[J]. Terrestrial, Atmospheric and Oceanic Sciences, 2008, 19(4): 389-401. doi: 10.3319/TAO.2008.19.4.389(IMAGES)
[11]	Diekmann B, Hofmann J, Henrich R, et al. Detrital sediment supply in the southern Okinawa Trough and its relation to sea-level and Kuroshio dynamics during the late Quaternary[J]. Marine Geology, 2008, 255(1-2): 83-95. doi: 10.1016/j.margeo.2008.08.001
[12]	Kawahata H, Ohshima H. Vegetation and environmental record in the northern East China Sea during the late Pleistocene[J]. Global and Planetary Change, 2004, 41(3-4): 251-273. doi: 10.1016/j.gloplacha.2004.01.011
[13]	叶银灿, 庄振业, 刘杜娟, 等.东海全新世沉积强度分区[J].青岛海洋大学学报, 2002, 32(6): 941-948. doi: 10.3969/j.issn.1672-5174.2002.06.010 YE Yincan, ZUANG Zhenye, LIU Dujuan, et al. Holocene depositional strength zoning in the East China Sea[J]. Journal of Qingdao Ocean University, 2002, 32(6): 941-948. doi: 10.3969/j.issn.1672-5174.2002.06.010
[14]	Yang Z S, Saito Y, Guo Z G, et al. Distal mud area as a material sink in the East China Sea[M].Japan:Hokkido University Press, 1994:1-6.
[15]	Ujiié Y, Ujiié H. Distribution and oceanographic relationships of modern planktonic foraminifera in the Ryukyu Arc region, Northwest Pacific Ocean[J]. The Journal of Foraminiferal Research, 2000, 30(4): 336-360. doi: 10.2113/0300336
[16]	李铁刚, 常凤鸣.冲绳海槽古海洋学[M].北京:海洋出版社, 2009:34-35. LI Tiegang, CHANG Fengming. Paleoceanography in the Okinawa Trough[M]. Beijing: Ocean press, 2009:34-35.
[17]	Schiebel R, Hemleben C. Planktic Foraminifers in the Modern Ocean[M]. Berlin: Springer Nature, 2017.
[18]	Bé A. An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera[M]. London: Academic Press, 1977, 1: 1-100.
[19]	Schmuker B, Schiebel R. Planktic foraminifers and hydrography of the eastern and northern Caribbean Sea[J]. Marine Micropaleontology, 2002, 46: 387-403. doi: 10.1016/S0377-8398(02)00082-8
[20]	Naidu P D, Malmgren B A. A High-resolution record of Late Quaternary upwelling along the Oman Margin, Arabian Sea based on planktonic foraminifera[J]. Paleoceanography, 1996, 11(1): 129-140. doi: 10.1029/95PA03198
[21]	Conan S H, Brummer G J. Fluxes of planktic foraminifera in response to monsoonal upwelling on the Somalia Basin margin[J]. Deep-Sea Research Ⅱ, 2000, 47: 2207-2227. doi: 10.1016/S0967-0645(00)00022-9
[22]	Schiebel R, Zeltner A, Treppke U F, et al. Distribution of diatoms, coccolithophores and planktic foraminifers along a trophic gradient during SW monsoon in the Arabian Sea[J]. Marine Micropaleontology, 2004, 51(3-4): 345-371. doi: 10.1016/j.marmicro.2004.02.001
[23]	Bé A, Tolderlund S D. Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian Oceans[J]. Micropaleontology of Oceans, 1971: 105-149.
[24]	Watkins J M, Mix A C, Wilson J. Living planktic foraminifera: tracers of circulation and productivity regimes in the central equatorial Pacific[J]. Deep Sea Research Part Ⅱ: Topical Studies in Oceanography, 1996, 43(4-6): 1257-1282. doi: 10.1016/0967-0645(96)00008-2
[25]	Reynolds L A, Thunell R C. Seasonal production and morphologic variation of neogloboquadrina pachyderma (ehrenberg) in the northeast Pacific[J]. Micropaleontology, 1986, 32(1): 1-18. doi: 10.2307/1485696
[26]	Ujiié H, Hatakeyam Y, Gu X X, et al. Upward decrease of organic C/N ratios in the Okinawa Trough cores: proxy for tracing the post-glacial retreat of the continental shoreline[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 165: 129-140. doi: 10.1016/S0031-0182(00)00157-7
[27]	Zheng X F, Li A C, Wan S M, et al. ITCZ and ENSO pacing on East Asian winter monsoon variation during the Holocene: Sedimentological evidence from the Okinawa Trough[J]. Journal of Geophysical Research: Oceans, 2014, 119(7): 4410-4429. doi: 10.1002/2013JC009603
[28]	Li T G, Xu Z K, Lim D, et al. Sr-Nd isotopic constraints on detrital sediment provenance and paleoenvironmental change in the northern Okinawa Trough during the late Quaternary[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 430: 74-84. doi: 10.1016/j.palaeo.2015.04.017
[29]	Jian Z M, Wang P X, Saito Y, et al. Holocene variability of the Kuroshio current in the Okinawa Trough, northwestern Pacific Ocean[J]. Earth and Planetary Science Letters, 2000, 184: 305-319. doi: 10.1016/S0012-821X(00)00321-6
[30]	Ujiié Y, Ujiié H, Taira A, et al. Spatial and temporal variability of surface water in the Kuroshio source region, Pacific Ocean, over the past 21000 years: evidence from planktonic foraminifera[J]. Marine Micropaleontology, 2003, 49(4): 335-364. doi: 10.1016/S0377-8398(03)00062-8
[31]	Kao S J, Lin F J, Liu K K. Organic carbon and nitrogen contents and their isotopic compositions in surficial sediments from the East China Sea shelf and the southern Okinawa Trough[J]. Deep Sea Research Part Ⅱ: Topical Studies in Oceanography, 2003, 50(6-7): 1203-1217. doi: 10.1016/S0967-0645(03)00018-3
[32]	Iseki K, Okamura K, Kiyomoto Y. Seasonality and composition of downward particulate fluxes at the continental shelf and Okinawa Trough in the East China Sea[J]. Deep-Sea Research Ⅱ, 2003, 50: 457-473. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=f469580e853f4132985ed1f276bfb911
[33]	Sautter L R, Thune R C. Seasonal variability in the ¹⁸O and ¹³C of planktonic foraminifera from an upwelling environment: sediment trap results from San Pedro Basin, southern California[J]. Paleoceanography, 1991, 6(3): 307-334. doi: 10.1029/91PA00385
[34]	Xu X D, Oda M. Surface-water evolution of the eastern East China Sea during the last 36000 years[J]. Marine Geology, 1999, 156: 285-304. doi: 10.1016/S0025-3227(98)00183-2
[35]	李枫, 吴立, 朱诚, 等.江汉平原12.76 cal. kaBP以来环境干湿变化的高分辨率研究[J].地理科学, 2012, 32(7): 878-884. http://www.cnki.com.cn/Article/CJFDTotal-DLKX201207017.htm LI Feng, WU Li, ZHU Cheng, et al. A high-resolution study of moisture evolution in the Jianghan Plain since 12.76 cal.kaBP[J]. Geography, 2012, 32(7): 878-884. http://www.cnki.com.cn/Article/CJFDTotal-DLKX201207017.htm
[36]	An Z S, Porter C S, Kutzbach E J, et al. Asynchronous Holocene optimum of the East Asian monsoon[J]. Quaternary Science Reviews, 2000, 19: 743-762. doi: 10.1016/S0277-3791(99)00031-1
[37]	王晓翠, 朱诚, 吴立, 等.湖北江汉平原JZ-2010剖面沉积物粒度特征与环境演变[J].湖泊科学, 2012, 24(3): 480-486. doi: 10.3969/j.issn.1003-5427.2012.03.022 WANG Xiaocui, ZHU Cheng, WU Li, et al. Grain-size characteristics and sedimentary environment change of JZ-2010 section in Jianghan Plain, Hubei Province[J]. Journal of Lake Sciences, 2012, 24(3): 480-486. doi: 10.3969/j.issn.1003-5427.2012.03.022
[38]	安芷生, 吴锡浩, 王苏民, 等.中国中东部全新世气候适宜期与东亚夏季风变迁[J].科学通报, 1993, 38(14): 1302-1305. http://www.cnki.com.cn/Article/CJFDTotal-KXTB199314013.htm AN Zhisheng, WU Xihao, WANG Sumin, et al. Holocene optimum in center and eastern China and the evolution of the East Asian monsoon[J]. Chinese Science Bulletin, 1993, 38: 1302-1305. http://www.cnki.com.cn/Article/CJFDTotal-KXTB199314013.htm
[39]	Li T G, Nan Q Y, Jiang B, et al. Formation and evolution of the modern warm current system in the East China Sea and the Yellow Sea since the last deglaciation[J]. Chinese Journal of Oceanology and Limnology, 2009, 27(2): 237-249. doi: 10.1007/s00343-009-9149-4
[40]	Ujiié Y, Asahi H, Sagawa T, et al. Evolution of the North Pacific Subtropical Gyre during the past 190ka through the interaction of the Kuroshio Current with the surface and intermediate waters[J]. Paleoceanography, 2016, 31: 1498-1513. doi: 10.1002/2015PA002914
[41]	Lin Y S, Wei K Y, Lin I T, et al. The Holocene Pulleniatina Minimum Event revisited: Geochemical and faunal evidence from the Okinawa Trough and upper reaches of the Kuroshio current[J]. Marine Micropaleontology, 2006, 59(3-4): 153-170. doi: 10.1016/j.marmicro.2006.02.003
[42]	Li T G, Liu Z X, Hall A M. Heinrich event imprints in the Okinawa Trough: evidence from oxygen isotope and planktonic foraminifera[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 176(1-4): 133-146. doi: 10.1016/S0031-0182(01)00332-7
[43]	Wu W X, Liu T S. Possible role of the "Holocene Event 3" on the collapse of Neolithic Cultures around the Central Plain of China[J]. Quaternary International, 2004, 117(1): 153-166. doi: 10.1016-S1040-6182(03)00125-3/
[44]	Sawada K, Handa N. Variability of the path of the Kuroshio Current over the past 25000 years[J]. Nature, 1998, 392: 592-595. doi: 10.1038/33391
[45]	Moy C M, Seltzer G O, Rodbell D T, et al. Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch[J]. Nature, 2002, 420(6912): 159-162. doi: 10.1038/nature01163
[46]	Sandweiss D H, Richardson J B, Reitz E J, et al. Geoarchaeological evidence from Peru for a 5000 Years B.P. onset of El Niño[J]. Science, 1996, 273: 1531-1533. doi: 10.1126/science.273.5281.1531

Cited By

Cited by

Periodical cited type(14)

1.	李建平，贾万丽，李宏义，张成，闫琢玉. 物源—地貌双控背景下海底扇沉积储层特征及勘探意义：以琼东南盆地梅山组为例. 地质科学. 2024(01): 148-165 .
2.	周荔青，江东辉，杨鹏程，张如凤，董鑫，桑亚迪. 琼东南盆地陵水北坡LS13-2区勘探思路与突破方向. 石油与天然气地质. 2024(03): 673-683 .
3.	刘子玉，贾万丽，李建平，刘为，武爱俊. 浊积扇沉积构成及主要单元储层差异:以琼东南盆地梅山组为例. 地质科学. 2024(05): 1268-1279 .
4.	吴克强，裴健翔，胡林，何小胡，金秋月. 莺歌海-琼东南盆地油气勘探新进展与思考. 中国海上油气. 2024(05): 1-13 .
5.	龚承林，徐长贵，尤丽，朱一杰. 深海重力流与底流交互作用的沉积响应及其勘探意义. 矿物岩石地球化学通报. 2024(04): 721-733+687 .
6.	龚胜利，闫琢玉，李百强，张铜耀，吴土荣，彭俊峰，郑磊，张东峰，黄向胜，罗程飞，王任. 琼东南盆地中中新统海底扇碎屑岩锆石U-Pb年龄特征及物源分析. 地质科技通报. 2024(05): 45-54 .
7.	熊连桥，谢晓军，唐武，白海强，刘子玉，于进鑫，陈莹. 琼东南盆地乐东凹陷梅山组海底扇发育异重流：来自岩心的证据. 海洋学报. 2024(12): 53-65 .
8.	欧阳杰，胡斌，杨金海，冷济高，邓盾. 琼东南盆地陵水凹陷S2井区梅山组物源. 成都理工大学学报(自然科学版). 2023(02): 200-205 .
9.	李建平，闫琢玉，徐微，刘景环. 琼东南盆地中央坳陷西北部梅山组浊积扇源-汇分析. 中国海上油气. 2023(03): 53-67 .
10.	李建平，熊连桥，黄琪斐，徐微，李祥权. 琼东南盆地梅山组浊积扇分类及其勘探意义. 油气地质与采收率. 2023(06): 1-12 .
11.	罗泉源，甘军，焦祥燕，胡潜伟，陈杨. 琼东南盆地深水区陵南低凸起潜山储层特征及控制因素. 天然气地球科学. 2023(12): 2101-2111 .
12.	郑秀娟，杜远生，朱筱敏，刘招君，胡斌，吴胜和，邵龙义，旷红伟，罗静兰，钟大康，李华，何登发，朱如凯，鲍志东. 中国古地理学近十年主要进展. 矿物岩石地球化学通报. 2021(01): 94-114+4 .
13.	尤丽，江汝锋，徐守立，詹冶萍，龚宇，郑飞，雷新. 琼东南盆地深水区乐东-陵水凹陷梅山组天然气成藏特征与勘探潜力. 中国海上油气. 2021(05): 24-31 .
14.	朱筱敏，董艳蕾，曾洪流，林承焰，张宪国. 中国地震沉积学研究现状和发展思考. 古地理学报. 2020(03): 397-411 .

Other cited types(2)

Get Citation

PDF

XML

Article views (2983) PDF downloads (41) Cited by(16)

Turn off MathJax

Article Contents

Abstract

References

The hydroclimate changes in the northern Okinawa Trough during middle Holocene: Evidence from planktonic foraminiferal assemblages