渤海湾西北岸牡蛎礁体对区域性构造活动与水动型海面变化的响应
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摘要
渤海湾地区广泛分布的古海面标志物,为建立该地区的相对海面变化曲线提供了良好的基础。过去 20年来该地区已相继建立了一些相对海面变化曲线,但在讨论影响古海面标志物高程的因素时,未将构造活动与水动型海面变化及均衡作用对高程的贡献量加以区分。文章以该地区 7个点的古海面标志物及相关层位的高程测量与年代学测定结果,经与地区性预测海面变化曲线进行对比后,定量讨论了该地区海面变化(包括绝对海面变化与冰川、水均衡作用)与构造活动对古海面标志物高程的贡献;并以壳体的稳定同位素、地层记录与古地震研究资料讨论了牡蛎礁体在建礁过程中所记录的构造下沉。
The widely scattered paleo-mean sea-level indicators along the Bohai Bay supply basic foundation for reconstructing of relative sea-level change in this area. During the past 20 years, scientists had built some relative sea-level curves in this area. However, they mixed all the impacting factors to the elevation of paleo-mean sea-level indicators up when they built this curves. A spatial-temporary distribution of such seven indicators, corresponding with the regional predicted sea-level curve, is established to calculate the subsidence of each indicator. Therefore, we can distinguish the contributions of tectonics and sea-level change associated with glacio- and hydro-isostatic adjustment in the local area to the elevations of the indicators. Furthermore, with the results of stable isotopic analyses to the oyster shells in the Biaokou reef and a paleo-earthquake trace in Dawuzhuang reef, we discuss the tectonic subsidence during the buildup of the reef bodies. And we compare the result to a strong paleo-earthquake event occurred in this area with spatial distribution map and 14C dating ages. As proxies, the results of oxygen and carbon isotopic analyses to the shells, lying on different vertical positions in one section, have indicated tectonic movements and subsidence recorded in the reef body while it was building up.
The widely scattered paleo-mean sea-level indicators along the Bohai Bay supply basic foundation for reconstructing of relative sea-level change in this area. During the past 20 years, scientists had built some relative sea-level curves in this area. However, they mixed all the impacting factors to the elevation of paleo-mean sea-level indicators up when they built this curves. A spatial-temporary distribution of such seven indicators, corresponding with the regional predicted sea-level curve, is established to calculate the subsidence of each indicator. Therefore, we can distinguish the contributions of tectonics and sea-level change associated with glacio- and hydro-isostatic adjustment in the local area to the elevations of the indicators. Furthermore, with the results of stable isotopic analyses to the oyster shells in the Biaokou reef and a paleo-earthquake trace in Dawuzhuang reef, we discuss the tectonic subsidence during the buildup of the reef bodies. And we compare the result to a strong paleo-earthquake event occurred in this area with spatial distribution map and 14C dating ages. As proxies, the results of oxygen and carbon isotopic analyses to the shells, lying on different vertical positions in one section, have indicated tectonic movements and subsidence recorded in the reef body while it was building up.
引文
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1)与王若柏的讨论.2004
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2)WangHong.PalaeoenvironmentofHolocenechenierandoysterreefsintheBohaiBay(China).PhDDissertation,VrijeUniversiteitBrussel,1994.1~249
1)WangHong.PalaeoenvironmentofHolocenechenierandoysterreefsintheBohaiBay(China).PhDDissertation,VrijeUniversiteitBrussel,1994.1~249
1)与王若柏的讨论.2004
2)WangHong.PalaeoenvironmentofHolocenechenierandoysterreefsintheBohaiBay(China).PhDDissertation,VrijeUniversiteitBrussel,1994.1~249
1)王 宏,阎玉忠,李建芬等.渤海湾牡蛎平原牡蛎礁形成与演化专题研究报告.2002.1~57
1 王 宏.渤海湾牡蛎礁与新构造活动———几个基本问题的讨论.见:卢演俦,高维明,陈国星等主编.新构造与环境.北京:地震出版社,2001.171~184WangHong.OysterreefsandneotectonicmovementsintheBohaiBay:Discussionofsomequestions.In:LuYanchou,GaoWeim ing,ChenGuoxingetal. eds.NeotectonismandEnvironment.Bei jing:SeismologicalPress,2001.171~184
2 赵希涛,耿秀山,张景文.中国东部20,000年来的海平面变化.海洋学报,1979,1(2):269~281ZhaoXitao,GengXiushan,ZhangJingwen.SealevelchangesineasternChinaduringthepast20,000years.ActaOceanologicaSini ca,1982,1(2):248~258
3 彭 贵,张景文,焦文强等.渤海湾沿海晚第四纪地层14C年代学研究.地震地质,1980,2(2):71~78PengGui,ZhangJingwen,JiaoWenqiangetal.ChronologyofLateQuaternarydepositsalongthecoastoftheBohaiBay.SeismologyandGeology,1980,2(2):71~78
4 李元芳,安凤桐.天津平原第四纪微古化石及其古地理意义.地理学报,1985,40(2):155~168LiYuanfang,AnFengtong.TheQuaternarymicropaleontologicalfossilsinTianjinPlainandtheirpaleogeographicsignificance.ActaGeographicaSinica,1985,40(2):155~168
5 李秀文,赵福利.14C数据(TD)I.见:中国第四纪研究委员会碳十四年代学组编.第四纪冰川与第四纪地质论文集(第六集)———碳十四专集.北京:地质出版社,1990.86~102LiXiuwen,ZhaoFuli.Radiocarbondata(TD)I.In:TheRadio carbonDatingSocietyofChineseQuaternaryResearchAssociationed.ContributiontotheQuaternaryGlaciologyandGeologyⅥ:Spe cialIssueon14CDating.Beijing:GeologicalPublishingHouse,1990.86~102
6 王 强,李秀文,张志良等.天津地区全新世牡蛎滩的古海洋学意义.海洋学报,1991,13(3):371~380WangQiang,LiXiuwen,ZhangZhiliangetal.Palaeo oceanologicalsignificanceinHoloceneostraceanbanksinTianjinarea.ActaOceanologicaSinica,1991,13(3):371~380
7 赵希涛,韩有松,李平日等.区域海岸演化与海面变化及其地质记录.见:施雅风总主编(赵希涛本卷主编).中国海面变化.济南:山东科学技术出版社,1996.52~70ZhaoXitao,HanYousong,LiPingrietal.Regionalcoastaldevel opment, sea levelchangeandtheirgeologicalrecords.In:ShiYafeng(ZhaoXitao)ed.ChinaSeaLevelChange.Jinan:Shan dongScience&TechnologyPress,1996.52~70
8 钟新宝,康 慧.渤海湾海岸带近现代地质环境变化.第四纪研究,2002,22(2):131~135ZhongXinbao,KangHui.Recentgeo environmentalchangesintheBohaiBayCoast.QuaternarySciences,2002,22(2):131~135
9 王 宏.渤海湾泥质海岸带近现代地质环境变化研究(Ⅰ):意义、目标与方法.第四纪研究,2003,23(4):385~392WangHong.Geo environmentalchangesontheBohaiBaymuddycoast(Ⅰ):Significance, goalsandmethods.QuaternarySciences,2003,23(4):385~392
10 王 宏.渤海湾泥质海岸带近现代地质环境变化研究(Ⅱ):成果与讨论.第四纪研究,2003,23(4):393~403WangHong.Geo environmentalchangesontheBohaiBaymuddycoast(Ⅱ):Resultsanddiscussions.QuaternarySciences,2003,23(4):393~403
11 SatoH,OkunoJ,KatohSetal.HolocenecrustalmovementalongthecoastofwesternKobeandthe1995KobeEarthquake,Japan.QuaternaryScienceReviews,2003,22(8~9):891~897
12 SatoH,OkunoJ,NakadaMetal.Holoceneupliftderivedfromrel ativesea levelrecordsalongthecoastofwesternKobe,Japan.Qua ternaryScienceReviews,2001,20(13):1459~1474
13 天津地质矿产局编.天津市区域地质志.北京:地质出版社,1992.189~220TianjinBureauofGeologyandMineralResourcesed.GeologicalBulletinofTianjinArea.Beijing:GeologicalPublishingHouse,1992.189~220
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15 SurgeDM,LohmannKC.DettmanDL.ControlsonisotopicchemistryoftheAmericanoyster,Crassostreavirginica:Implicationsforgrowthpatterns.Palaeogeography,Palaeoclimatology,Palaeo ecology,2001,172:283~296
16 SurgeDM,LohmannKC,GoodfriendGA.Reconstructingestuar ineconditions:Oystershellsasrecordersofenvironmentalchange,SouthwestFlorida.Estuarine,CoastalandShelfScience,2003,57:737~756
17 张忍顺.江苏小庙洪牡蛎礁的地貌-沉积特征.海洋与湖沼,2004,35(1):1~7ZhangRenshun.Thegeomorphology sedimentologycharacterofoys terreefinXiaomiaohongtidalchannel,JiangsuProvince.Oceanolo giaetLimnologicaSinica,2004,35(1):1~7
18 T nqvistTE,MarkHMvanRee,Ronvan tVeeretal.Improvingmethodologyforhigh resolutionreconstructionofsea levelriseandneotectonicsbypaleocologicalanalysisandAMS14Cdatingofbasalpeats.QuaternaryResearch,1998,49(1):72~85
19 赵希涛,杨达源等编.全球海面变化.北京:科学出版社,1992.1~55ZhaoXitao,YangDayuanetal. eds.GlobeSeaLevelChanges.Beijing:SciencePress,1992.1~55
20 ClarkJA,FarrellWE,PeltierWR.Globalchangesinpostglacialsealevel:Anumericalcalculation.QuaternaryResearch,1978,9(3):265~287
21 李凤林,王 宏,阎玉忠等.渤海湾西岸滨海平原晚第四纪以来的沉积间断.地质调查与研究,2004,27(3):177~183LiFenglin,WangHong,YanYuzhongetal.ThesignificanceofthedepositionalhiatusesonthecoastalplainofWestBohaiBaysincetheLateQuaternaryperiod.GeologicalSurveyandResearch,2004,27(3):177~183
22 王 宏,李凤林,范昌福等.环渤海海岸带14C数据集(Ⅰ).第四纪研究,2004,24(6):601~613WangHong,LiFenglin,FanChangfuetal.The14Cdatabase(I)ontheCircumBohaiSeaCoast.QuaternarySciences,2004,24(6):601~613
23 StuiverM,ReimerPJ,BardEetal.INTCAL98radiocarbonagecalibration24,000~0BP.Radiocarbon,1998,40:1041~1083
24 StuiverM,ReimerPJ,ReimerR.CALIB4.1~4.4Manuals.2003(http://www.calib.org)
25 SouthonJ,KashgarianM,FontugneMetal.Marinereservoircor rectionsfortheIndianOceanandSoutheastAsia.Radiocarbon,2002,44:167~180
26 PirazzoliPA.Sea levelchange.NatureandResourcesⅩⅪ,1985,4:2~10
27 NakadaM,OkunoJ,YokoyamaYetal.MidHoloceneunderwaterJomonsitesalongthewestcoastofKyushu,Japan, andastheno sphericviscosity.TheQuaternaryResearch(Japanese),1998,37:315~323
28 NakadaM,LambeckK.ThemeltinghistoryoftheLatePleistoceneAntarcticicesheet.Nature,1988,333(5):36~40
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