Sedimentary environment and evaluation of oyster reef in Liyashan, Haimen, Jiangsu Province
-
摘要:
为了解江苏海门蛎岈山牡蛎礁沉积状况及其环境特征,于2023年对该区沉积物进行了垂直剖面柱样采样,并开展了粒度统计分析及210Pb和137Cs测年。结果表明,江苏海门蛎岈山牡蛎礁发育底质为砂质粉砂和粉砂。C01柱样的总210Pb活度和过剩210Pbex活度两者之间的变化趋势基本相同,呈“衰减层-本底层”二段式;而C02柱样呈“混合层-本底层”二段式,其表层混合层0~70 cm有波动变化,70 cm以下大体处于相对稳定状态。研究区南部总体受到侵蚀,北部有一定的淤积。近岸区受沿岸流、潮汐、潮流共同作用,水动力较强;远岸区水体较深,潮汐作用较弱,水动力条件弱,沉积速率较小。本研究对于当地开展牡蛎礁保护和生态修复以及调整保护区边界具有重要的指导意义。
Abstract:To understand the sedimentation and environmental characteristics in oyster reefs in Liyashan, Haimen, Jiangsu, vertical column sampling of sediments was carried out in 2023, from which the grain size statistical analysis, and 210Pb and 137Cs dating of sediments were conducted. Results indicate that the substrate of the oyster reef consists of sandy silt and silt. The 210Pb activity and excess 210Pbex activity in core C01 exhibit a similar trend, characterized by a "decay layer - background layer" dual structure. In contrast, core C02 displays a "mixing layer–background layer" dual structure; the top 0-70 cm is the mixing layer, showing fluctuations in the activities, while below 70 cm, the activities remain relatively stable. The southern part of the study area is generally subject to erosion, while the northern part shows some siltation. Nearshore samples are influenced by the combined effects of coastal currents, tides, and tidal flows, resulting in stronger hydrodynamic conditions. In offshore areas, deeper waters and weaker tidal forces lead to less dynamic conditions and lower sedimentation rates. This study has important practical significance for local oyster reef protection and ecological restoration, as well as for the adjustment of the boundaries of protected areas.
-
Key words:
- intertidal zone /
- oyster reef /
- sedimentary environment /
- environmental monitoring
-
-
表 1 沉积柱粒度参数统计
Table 1. Statistics of particle size parameters of the sediment samples
样品编号 深度/cm 平均粒径/Φ 分选系数 偏态 峰度 砂/% 粉砂/% 黏土/% C01-L1 0~5 5.74 1.39 0.18 2.30 6.81 84.23 8.96 C01-L2 10~15 5.72 1.45 0.10 2.31 8.1 82.52 9.38 C01-L3 20~25 5.30 1.81 −0.02 2.19 22.42 67.71 9.87 C01-L4 30~35 6.00 1.53 −0.13 2.31 7.49 78.4 14.11 C01-L5 40~45 6.13 1.49 −0.22 2.58 5.51 79.24 15.25 C01-L6 50~55 6.32 1.35 −0.14 2.39 2.72 81.05 16.23 C01-L7 60~65 6.27 1.49 −0.32 2.64 5.12 77.58 17.3 C01-L8 70~75 6.21 1.49 −0.21 2.41 5.43 77.79 16.78 C01-L9 80~85 5.88 1.48 0.09 2.21 6.79 80.96 12.25 C01-L10 90~95 5.85 1.55 −0.03 2.19 8.94 78.37 12.69 C01-L11 100~105 4.24 1.28 1.23 4.76 37.79 59.71 2.5 C01-L12 110~115 3.87 1.15 0.73 5.08 46.68 52.49 0.83 C02-L1 0~5 2.66 1.54 1.77 5.99 84.77 13.79 1.44 C02-L2 10~15 2.59 1.08 2.34 10.63 93.39 6.09 0.52 C02-L3 20~25 3.19 1.66 1.22 4.03 74.05 23.99 1.96 C02-L4 30~35 4.37 1.92 0.26 2.22 41.46 53.71 4.83 C02-L5 40~45 4.91 1.72 0.14 2.28 27.97 66.39 5.64 C02-L6 50~55 3.41 1.62 1.11 3.71 68.63 29.48 1.89 C02-L7 60~65 5.55 1.37 0.32 2.34 8.26 84.33 7.41 C02-L8 70~75 5.63 1.43 0.20 2.49 7.85 83.38 8.77 C02-L9 80~85 5.51 1.38 0.17 2.60 8.75 84.6 6.65 C02-L10 90~95 5.43 1.49 0.14 2.30 13.57 79.32 7.11 C02-L11 100~105 5.44 1.57 −0.02 2.47 14.32 77.97 7.71 C02-L12 110~115 5.43 1.54 0.03 2.48 13.69 78.95 7.36 C02-L13 120~125 4.88 1.74 0.14 2.30 28.63 65.66 5.71 C02-L14 130~134 5.58 1.39 0.18 2.60 7.64 84.85 7.51 表 2 210Pb和137Pb样品检测结果
Table 2. Results of 210Pb和137Pb measurement of the samples
样品编号 深度/cm 210Pb/(Bq/kg) 226Ra/(Bq/kg) 137Cs/(Bq/kg) C01-2 2~4 51.9±3.1 31.3±1.4 <0.85 C01-4 6~8 48.3±2.9 30.3±1.3 <0.66 C01-6 10~12 54.4±3.0 28.2±1.2 <0.64 C01-10 18~20 39.7±2.7 29.0±1.2 <0.60 C01-14 26~28 45.9±3.1 35.5±1.4 <0.71 C01-16 30~32 50.3±3.2 43.8±1.6 <0.70 C01-19 36~38 49.7±2.9 40.2±1.4 <0.62 C01-21 40~42 44.7±3.0 41.3±1.5 <0.66 C01-24 46~48 43.7±2.7 38.5±1.4 <0.58 C01-26 50~54 44.6±2.7 39.0±1.3 <0.43 C01-27 54~58 40.9±2.6 36.8±1.2 <0.48 C01-29 62~66 43.0±2.6 42.3±1.3 <0.41 C01-32 74~78 41.3±2.7 41.5±1.3 <0.43 C02-2 2~4 40.4±3.4 22.0±1.1 <1.06 C02-4 6~8 29.9±3.2 23.1±1.0 <0.88 C02-6 10~12 36.5±3.3 22.8±1.1 <0.99 C02-10 18~20 31.5±3.3 25.6±1.2 <0.98 C02-14 26~28 44.4±3.5 34.1±1.3 <0.88 C02-19 36~38 31.1±2.7 25.8±0.9 <0.67 C02-24 46~48 36.2±3.1 24.5±1.0 <0.84 C02-27 54~58 31.1±2.7 24.8±0.9 <0.51 C02-30 66~70 59.4±3.3 32.1±1.1 <0.64 C02-33 78~82 40.5±2.9 29.7±1.0 <0.51 C02-36 90~94 36.0±3.1 26.5±1.0 <0.79 C02-40 110~120 37.3±2.8 28.8±0.9 <0.54 注:1 Bq/kg=60 dpm/kg =60/ 1000 dpm/g。 -
[1] COEN L D,LUCKENBACH M W. Developing success criteria and goals for evaluating oyster reef restoration:ecological function or resource exploitation[J]. Ecological Engineering,2000,15(3):323-343
[2] The Nature Conservancy (TNC) China Program. Oyster reef ecosystem engineer[J]. Man and the Biosphere,2020,1:30-32.
[3] NELSON K A,LEONARD L A,POSEY M H,et al. Using transplanted oyster (Crassostrea virginica) beds to improve water quality in small tidal creeks:a pilot study[J]. Journal of Experimental Marine Biology and Ecology,2004,298(2):347-368. doi: 10.1016/S0022-0981(03)00367-8
[4] DAME R F,BUSHEK D,ALLEN D M,et al. The experimental analysis of tidal creeks dominated by oyster reefs:the premanipulation year[J]. Journal of Shellfish Research,2000,19(1):361-369.
[5] MILLER A W,REYNOLDS A C,SOBRINO C,et al. Shellfish face uncertain future in high CO2 world:influence of acidification on oyster larvae calcification and growth in estuaries[J]. PloS One,2009,4(5):5661. doi: 10.1371/journal.pone.0005661
[6] 庄佳铨,罗科,彭雲,等. 基于无人机SfM 摄影测量的潮间带牡蛎礁地貌调查[J]. 海洋地质与第四纪地质,2023,43(6):45-54.
ZHUANG J Q,LUO K,PENG Y,et al. Geomorphology investigation of intertidal oyster reef based on unmanned aerial vehicle SfM photogrammetry[J]. Marine Geology & Quaternary Geology,2023,43(6):45-54.
[7] 张忍顺. 江苏小庙洪牡蛎礁的地貌-沉积特征[J]. 海洋与湖沼,2004,35(1):1-7. doi: 10.3321/j.issn:0029-814X.2004.01.001
ZHANG R S. Geomorphological and sedimentary characteristics of Xiaomiaohong oyster reef in Jiangsu Province[J]. Oceanologia et Limnologia Sinica,2004,35(1):1-7. doi: 10.3321/j.issn:0029-814X.2004.01.001
[8] 项立辉,王艳芬,姜辞冬,等. 江苏中部潮间带表层沉积物重金属分布、来源及污染评价[J]. 海洋地质前沿,2024,40(8):42-52.
XIANG L H,WANG Y F,JIANG C D,et al. Distribution,origin and pollution evaluation of heavy metals in surface sediments of intertidal zone in central Jiangsu[J]. Marine Geology Frontiers,2024,40(8):42-52.
[9] 全为民,周为峰,马春艳,等. 江苏海门蛎岈山牡蛎礁生态现状评价[J]. 生态学报,2016,36(23):7749-7757.
QUAN W M,ZHOU W F,MA C Y,et al. Assessment on the ecological status of the oyster reef in Liyashan Mountain,Haimen,Jiangsu Province[J]. Acta Ecologica Sinica,2016,36(23):7749-7757.
[10] 李路路,鲍宽乐,张家强,等. 湛江湾-雷州湾海域表层沉积物中底栖有孔虫分布特征及其环境意义[J]. 海洋地质前沿,2024,40(11):46-56.
LI L L,BAO K L,ZHANG J Q,et al. Distribution characteristics of benthic foraminifera in surface sediments of Zhanjiang Bay and Leizhou Bay and its environmental significance[J]. Marine Geology Frontiers,2024,40(11):46-56.
[11] 孙万胜,温国义,白明,等. 天津大神堂浅海活牡蛎礁区生物资源状况调查分析[J]. 河北渔业,2014(9):23-26. doi: 10.3969/j.issn.1004-6755.2014.09.008
SUN W S,WEN G Y,BAI M,et al. Investigation and analysis of biological resources in the living oyster reef area in the shallow-sea of Dashentang,Tianjin[J]. Hebei Fisheries,2014(9):23-26. doi: 10.3969/j.issn.1004-6755.2014.09.008
[12] JOHNSON K D,SMEE D L. Predators influence the tidal distribution of oysters[J]. Marine Biology,2014,161(7):1557-1564. doi: 10.1007/s00227-014-2440-8
[13] 王建,赵梅,白世彪,等. 黄海南部海门近岸牡蛎礁发育的物质基础与环境背景[J]. 地理研究,2009,28(5):1170-1178. doi: 10.3321/j.issn:1000-0585.2009.05.003
WANG J,ZHAO M,BAI S B,et al. Physical basis and environmental background of the development of offshore oyster reefs in Haimen,southern Yellow Sea[J]. Geographical Research,2009,28(5):1170-1178. doi: 10.3321/j.issn:1000-0585.2009.05.003
[14] 方晶,王宏,王福,等. 渤海湾西北岸埋藏牡蛎礁礁顶上下沉积物中硅藻对“礁泥转换”古沉积环境的重建[J]. 沉积学报,2012,30(5):879-890.
FANG J,WANG H,WANG F,et al. Reconstruction of the paleo-sedimentary environment of "reef-mud conversion" by diatoms in the sediments below the roof of buried oyster reef in northwest coast of Bohai Bay[J]. Acta Sedimentologica Sinica,2012,30(5):879-890.
[15] 范昌福,高抒,王宏. 渤海湾西北岸全新世埋藏牡蛎礁建造记录中的间断及其解释[J]. 海洋地质与第四纪地质,2006,26(5):27-35.
FAN C F,GAO S,WANG H. Interperting the hiatus in holocene oyster reefs on the northwest coast of Bohai Bay[J]. Marine Geology & Quaternary Geology,2006,26(5):27-35.
[16] 范昌福,王宏,裴艳东,等. 渤海湾西北岸滨海湖埋藏牡蛎礁古生态环境[J]. 海洋地质与第四纪地质,2008,28(1):33-41.
FAN C F,WANG H,PEI Y D,et al. Palaeoecological environment revealed by the nuried binhaihu oyster reef on the northwest coast of Bohai Bay[J]. Marine Geology & Quaternary Geology,2008,28(1):33-41.
[17] 方晶,胡克,范昌福,等. 渤海湾西北岸滨海湖埋藏牡蛎礁硅藻及其记录的古环境[J]. 海洋地质与第四纪地质,2012,32(5):81-88.
FANG J ,HU K,FAN C F,et al. Diatom records of the binhu buried otster reef,in Binhaihu northwest Bohai Bay and paleo-environmental implications[J]. Marine Geology & Quaternary Geology,2012,32(5):81-88.
[18] 刘秀明,李文宝,邢春额. MS2000激光粒度分析仪在沉积物分析中的应用[J]. 实验技术与管理,2007,24(9):49-52. doi: 10.3969/j.issn.1002-4956.2007.09.015
LIU X M,LI W B,XING C E. Application of MS2000 laser particle size analyzer in sediment analysis[J]. Experimental Technology and Management,2007,24(9):49-52. doi: 10.3969/j.issn.1002-4956.2007.09.015
[19] MCMANUS J. Grain Size Determination and Interpretation [M]. Oxford:Blackwell,1988:63-85.
[20] FOLK R L,ANDREWS P B,LEWIS D W. Detrital sedimentary rock calssification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysics,1970,13(4):937-968. doi: 10.1080/00288306.1970.10418211
[21] 王君波,朱立平,汪勇. 西藏纳木错现代沉积速率的空间分布特征及近60年来的变化研究[J]. 第四纪研究,2011,31(3):535-543. doi: 10.3969/j.issn.1001-7410.2011.03.17
WANG J B,ZHU L P,WANG Y. Study on the spatial distribution characteristics of modern sedimentation rate in Namco,Tibet and its changes in recent 60 years[J]. Quaternary Sciences,2011,31(3):535-543. doi: 10.3969/j.issn.1001-7410.2011.03.17
[22] 王颖. 黄海陆架辐射沙脊群[M]. 北京:中国环境科学出版社:2002,119-228.
WANG Y. Radiating Sand Ridge Group of the Yellow Sea Shelf [M]. Beijing:China Environmental Science Press:2002,119-228.
[23] 吉会峰,李用留,高清清,等. 基于地波雷达观测资料的烂沙洋海域表层海流特征研究[J]. 海洋预报,2017,34(5):64-73. doi: 10.11737/j.issn.1003-0239.2017.05.007
JI H F,LI Y L,GAO Q Q,et al. Based on the observation data of ground wave radar shayang characteristics of sea surface current study[J]. Marine Forecast,2017,34(5):64-73. doi: 10.11737/j.issn.1003-0239.2017.05.007
[24] 陈蕴真,高抒. 江苏南部海岸牡蛎礁演化的几何模型[J]. 海洋与湖沼,2010,41(1):1-11. doi: 10.11693/hyhz201001001001
CHEN Y Z,GAO S. Geometric model of oyster reef evolution in southern Jiangsu coast[J]. Oceanologia et Limnologia Sinica,2010,41(1):1-11. doi: 10.11693/hyhz201001001001
[25] 朱诚,卢春成. 长江三角洲及苏北沿海地区7000年以来海岸线演变规律分析[J]. 地理科学,1996(3):207-214.
ZHU C,LU C C. The Yangtze River Delta and coastal areas of north Jiangsu coastline evolution analysis since 7 000 years[J]. Scientia Geographica Sinica,1996(3):207-214.
[26] 褚欲良. 南黄海辐射沙洲形成发育动力机制研究I. 潮流运动平面特征[J]. 中国科学(D辑),1998,28(5):403-410.
CHU Y L. Study on the dynamic mechanism of formation and development of radiating sandbanks in the South Yellow Sea I. Plane characteristics of tidal currents [J].Science in China (Series D),1998,28(5):403-410.
-