陆相盆地古生产力研究现状Current Status of Paleoproductivity Research in Continental Basins
胡玮;卢宗盛;喻鹏;
摘要(Abstract):
古生产力是指地质历史时期生物在能量循环过程中固定能量的速率。陆相盆地古生产力的研究包括古生产力的大小及其组成研究两个方面。目前主要通过有机碳、生物硅和生物标志化合物等指标来评估陆相盆地古生产力的大小;通过生物标志化合物指标,包括正烷烃、萜类、甾类分子标志化合物等指标来研究陆相盆地古生产力的组成。陆相盆地古生产力的定量化研究比较欠缺,仅在有机碳、生物硅及生物标志化合物指标方面建立了数学模型,且多是对海相盆地古生产力指标的直接沿用;而在色素、湖相碳酸盐等具陆相特点的指标方面仅见部分定性研究。在地学应用方面,以陆相盆地古生产力研究为基础的地球生物学方法,在正演陆相烃源岩的形成过程研究中具有良好的前景。
关键词(KeyWords): 陆相盆地;古生产力;烃源岩评价
基金项目(Foundation): 国家科技重大专项(2009ZX05009-002;2008ZX05006-003)
作者(Author): 胡玮;卢宗盛;喻鹏;
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DOI:
参考文献(References):
- [1]Muller P J,Suess E.Productivity,sedi mentation rate,andsedi mentary organic matter in the oceans:1.Organic carbonpreservation[J].Deep-Sea Research,1979,26(12):1 347-1 362.
- [2]Van Kreveld S A,Knappertsbusch M,Ottens J,et al.Biogeniccarbonate and ice-rafted debris(Heinrich layer)accumulationin deep-sea sedi ments from a Northeast Atlantic piston core[J].Marine Geology,1996,131(1/2):21-46.
- [3]Brummer GJ A,van Eijden AJ M.“Blue-ocean”Paleoproduc-tivity esti mates frompelagic carbonate mass accumulation rates[J].Marine Micropaleontology,1992,19(1/2):99-117.
- [4]陈建芳.古海洋研究中的地球化学新指标[J].地球科学进展,2002,17(3):402-410.
- [5]刘传联,成鑫荣,王汝建,等.西太平洋暖池区第四纪钙质超微化石氧碳同位素特征及意义[J].地球科学:中国地质大学学报,2005,30(5):560-603.
- [6]陈木宏,黄良民,涂霞,等.南海放射虫与初级生产力的古海洋学转换关系[J].科学通报,1999,44(3):327-333.
- [7]Herguera J C.Last glacial paleoproductivity patterns in theeastern equatorial Pacific:Benthic foraminifera records[J].Marine Micropaleontology,2000,40(3):259-275.
- [8]倪建宇,张美,周怀阳.赤道东太平洋沉积物中生物钡的分布特征[J].海洋地质与第四纪地质,2006,26(2):49-54.
- [9]任景玲,张经,刘素美.Al/Ti比值为地球化学示踪剂反演海洋古生产力的研究进展[J].地球化学进展,2005,20(12):1 314-1 320.
- [10]Supriyo K D,Joyanto R,Alakendra N,et al.Major and traceelement geochemistry in Zeekoevlei,south Africa:A lawse-trine record of present and past processes[J].Applied Geo-chemistry,2008,23(8):2 496-2 511.
- [11]胡超涌,潘涵香,马仲武,等.海相碳酸盐岩中的铁:烃源岩古生产力评估的新指标[J].地球科学:中国地质大学学报,2007,32(6):755-758.
- [12]南青云,李铁刚,陈金霞,等.南冲绳海槽7000 a B.P.以来基于长链不饱和烯酮指标的古海洋生产力变化及其与气候的关系[J].第四纪研究,2008,28(3):482-490.
- [13]Hunt J M.Petrdeum geochemistry and geology[M].SanFrarscico:W.H.Freeman and Company,1979.
- [14]李守军,郑德顺,耿福兰.定量再造湖泊古生产力的尝试[J].高校地质学报,2002,8(2):215-219.
- [15]Ishi watari R,Negishi K,Yoshikawa H,et al.Glacial-inter-glacial productivity and environmental changes in Lake Bi wa,Japan:Asedi ment core study of organic carbon,chlorins andbiomarkers[J].Organic Geochemistry,2009,40(4):520-530.
- [16]刘传联,徐金鲤.生油古湖泊生产力的估算方法及应用实例[J].沉积学报,2002,20(1):144-149.
- [17]李守军,王纪存,郑德顺,等.东营凹陷沙河街组一段沉积时期的湖泊古生产力[J].石油与天然气地质,2004,25(6):656-658.
- [18]Prokopenko A A,Hinnov L A,Williams D F,et al.Orbitalforcing of continental cli mate during the Pleistocene:A com-plete astronomically tuned cli matic record from Lake Baikal,SE Siberia[J].Quaternary Science Reviews,2006,25(23/24):3 431-3 457.
- [19]Johnson T C,Brown E T,Shi J.Biogenic silica deposition inLake Malawi,East Africa over the past 150,000 years[J/OL].Palaeogeography,Palaeocli matology,Palaeoecology,2010,doi:10.1016/j.palaeo.2010.01.024.
- [20]Xiao J,Inouchi Y,Kumai H,et al.Biogenic silica record inLake Bi wa of Central Japan over the past 145,000 years[J].Quaternary Research,1997,47(3):277-283.
- [21]Levina O V,Karabanov E B.Modern accumulation rates of bio-genic silica in Baikal bottom sedi ments:Significance of diatomspecies composition[J].Russian Geology and Geophysics,2007,48(6):483-490.
- [22]杨群.分子古生物学原理与方法[M].北京:科学出版社,2003:96-97.
- [23]Castaneda I S,Weme J D,Johnson T J,et al.Organic geo-chemical records from Lake Malawi(East Africa)of the last700 years.Part II:Biomarker evidence for recent changes inpri mary productivity[J/OL].Palaeogeography,Palaeocli-matology,Palaeoecology,2010,doi:10.1016/j.palaeo.2010.01.006.
- [24]张枝焕,杨藩,李东明,等.中国新生界咸化湖相有机地球化学研究进展[J].地球科学进展,2000,15(1):65-70.
- [25]王铁冠,盛国英,陈军红,等.甲基三环菇烷与甲基四环菇烷的鉴定及其生源意义[J].科学通报,1994,39(10):933-935.
- [26]Zi mmerman A R,Canuel E A.Sedi ment geochemical recordsof eutrophicationin the mesohaline Chesapeake Bay[J].Li m-nology and Oceanography,2002,47(4):1 084-1 093.
- [27]Grossi V,Blokker P,Sinninghe-Damst J S.Anaerobic biodeg-radation of lipids of the marine microalga Nannochloropsis sali-na[J].Organic Geochemistry,2001,32(6):795-808.
- [28]刘传联,徐金鲤,汪品先.藻类勃发湖相油源岩形成的一种重要机制[J].地质评论,1993,47(2):207-210.
- [29]Meyers P A,Ishi watari R.Lacustrine organic geochemistry:An overview of indicators of organic matter sources and dia-gensis in lake sedi ments[J].Organic Geochemistry,1993,20(7):867-900.
- [30]金芳,黄俊华,汤新燕,等.梁子湖沉积物有机质碳同位素特征及其古气候指示意义[J].地质科技情报,2007,26(3):13-18.
- [31]Wanders J WB.The role of benthic algaeinthe shallowreef ofCuracao(Netherlands antilles)II:Pri mary productivity of theSargassumbeds on the north-east coast submarine plateau[J].Aquatic Botany,1976,2:327-335.
- [32]吴国?,朱伟林,黄正吉,等.湖相沉积浮游藻类及有机质类型与烃源研究[J].同济大学学报,1998,26(2):176-179.
- [33]秦养民,顾延生,王银善,等.天鹅洲长江故道近代环境变化的有壳变形虫记录[J].地质科技情报,2007,26(3):37-42.
- [34]Swain B.Measurement and interpretation of sedi mentary pig-ments[J].Freshwater Biology,1985,15(1):53-75.
- [35]Reuss N,Conley D J,Bianchi T S.Preservation conditions andthe use of sedi ment pigments as a tool for recent evological re-constructionin four Northern European estuaries[J].MarineChemistry,2005,95(3/4):283-302.
- [36]瞿文川,吴瑞金,王苏民,等.近2600年来内蒙古居延海湖泊沉积物的色素含量及环境意义[J].沉积学报,2000,18(1):13-17.
- [37]薛滨,潘红玺,夏威岚,等.历史时期希门错湖泊沉积色素记录的古环境变化[J],湖泊科学,1997,9(4):295-299.
- [38]吴生才,陈伟民.太湖浮游植物生物量的周期性变化[J].中国环境科学,2004,24(2):151-154.
- [39]王铁冠,钟宁宁,侯读杰,等.陆相湖盆生物类脂物早期生烃机制研究[J].中国科学:D辑,1996,26(6):518-524.
- [40]Meyers P A.Applications of organic geochemistry to paleoli m-nological reconstructions:A summary of examples from theLaurentian Great Lakes[J].Organic Geochemisty,2003,34(2):261-289.
- [41]宋宁,王铁冠,李美俊.江苏金湖凹陷古近系奇碳优势和偶碳优势共存的正构烷烃[J].沉积学报,2007,25(2):307-313.
- [42]程克明,王铁冠,钟宁宁,等.烃源岩地球化学[M].北京:科学出版社,1995.
- [43]Ficken J,Li B,Swain D L,et al.An alkane proxy for the sedi-mentary input of submerged/floating fresh water aquatic mac-rophytes[J].Organic Geochemistry,2000,31(7/8):745-749.
- [44]Peters K E,Moldowan J M.Biomarkers guide:Interpretingmolecular fossils in petroleum[M].[S.l.]:Prentice HallInc.,1993.
- [45]傅家谟,陈德玉,刘德汉,等.茂名油页岩中生物输入的标志化合物[J].地球化学,1985(2):99-113.
- [46]Brassell S C,Eglinton G,Fu Jiamo.Biological marker com-pounds as indicators of dipositional history of Maoming oilshale[J].Organic Geochemistry,1986,10(4/6):927-942.
- [47]傅家谟,盛国英.中国分子有机地球化学研究进展[J].沉积学报,1992,10(3):4-10.
- [48]盛国英,傅家谟,刘德汉.富含与泥盆系角质残植煤中的四环二萜烷[J].石油与天然气地质,1991,12(2):107-116.
- [49]王铁冠,盛国英,陈军红,等.甲基三环菇烷与甲基四环菇烷的鉴定及其生源意义[J].科学通报,1994,39(10):933-935.
- [50]张枝焕,杨藩,李东明,等.中国新生界咸化湖相有机地球化学研究进展[J].地球科学进展,2000,15(1):65-70.
- [51]王铁冠,侯读杰.板桥凹陷泥岩与原油中藿烷类的分布型式[J].科学通报,1994,39(1):61-64.
- [52]尚慧芸,姜乃煌.陆相原油及生油岩中的奥利烷及其地质意义[J].石油学报,1984,5(4):37-42.
- [53]王铁冠.生物标志物地球化学研究[M].武汉:中国地质大学出版社,1990:55-65.
- [54]张立平,黄第藩,廖志勤.伽马蜡烷:水体分层的地球化学标志[J].沉积学报,1999,17(1):136-140.
- [55]张枝焕,杨藩,方朝亮.我国第三系咸化湖相有机质组成及环境意义[J].西安石油学院学报,2002,17(6):16-24.
- [56]Peters K E,Moldowan J M.The biomarker guide:Interpretingmolecular fossils in petroleumand ancient sedi ments[M].En-glewood Cliffs,NewJersey:Prentice Hall,1993.
- [57]侯读杰,王铁冠.陆相湖盆沉积物和原油中的甲藻甾烷[J].科学通报,1995,40(4):333-335.
- [58]侯读杰,王铁冠,张一伟,等.中国东部第三系陆相沉积中的甲藻甾烷:海侵指相的标志物?[J].地质论评,1997,43(5):524-528.
- [59]王广利,张林哗,王铁冠.3β烷基甾烷在中国古近系陆相沉积中的发现及其地质意义[J].科学通报,2006,51(12):1 438-1 442.
- [60]Majone M,Massanisso P,Ramadori R.Comparison of carbonstorage under aerobic and anoxic conditions[J].Water Scienceand Technology,1998,38(8/9):77-84.
- [61]Bralower T J,Thierstein H R.Low productivity and slowdeep-water circalation in mid-cretaceous oceaus[J].Geology,1984,12:614-618.
- [62]Halbach M,Koschinsky A,Halbach P.Reporton the discov-ery of Gallionella ferruginea froman active hydrothermal fieldin the deep sea[J].International Ridge-Crest Reseach,2001,10(1):18-20.
- [63]熊志方,胡超涌,黄俊华,等.氧的非质量同位素分馏及其地学应用[J].地质科技情报,2007,26(2):51-57.
- [64]谢树成,殷鸿福,解习农,等.地球生物学方法与海相优质烃源岩形成过程的正演和评价[J].地球科学:中国地质大学学报,2007,32(6):727-740.
- [65]金之钧,龙胜祥,周雁,等.中国南方膏盐岩分布特征[J].石油与天然气地质,2006,27(5):572-59.