[1] Veizer J, Bruckschen P, Pawellek F, et al. Oxygen isotope evolution of Phanerozoic seawater[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1997, 132(1/2/3/4): 159-172.
[2] Veizer J, Buhl D, Diener A, et al. Strontium isotope stratigraphy: potential resolution and event correlation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1997, 132(1/2/3/4): 65-77.
[3] Brand U. Carbon, oxygen and strontium isotopes in Paleozoic carbonate components: an evaluation of original seawater-chemistry proxies[J]. Chemical Geology, 2004, 204(1/2): 23-44.
[4] Buggisch W, Joachimski M M. Carbon isotope stratigraphy of the Devonian of Central and Southern Europe[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 240(1/2): 68-88.
[5] 陈代钊,王卓卓,汪建国. 晚泥盆世地球各圈层相互作用与海洋生态危机:来自高分辨率的沉积和同位素地球化学证据[J]. 自然科学进展,2006,16(4):439-448.[Chen Daizhao, Wang Zhuozhuo, Wang Jianguo. The interactions of each layer in Earth and the crisis of marine ecological in Late Devonian:the evidence from the high resolution sedimentary and isotope values[J]. Progress in Natural Science, 2006, 16(4): 439-448.]
[6] Veizer J, Hoefs J. The nature of O18/O16 and C13/C12 secular trends in sedimentary carbonate rocks[J].Geochimica et Cosmochimica Acta, 1976, 40(11): 1387-1395.
[7] Killingley J S. Effects of diagenetic recrystallization on18O/16O values of deep-sea sediments[J]. Nature, 1983, 301(5901): 594-597.
[8] Veizer J, Ala D, Azmy K, et al.87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater[J]. Chemical Geology, 1999, 161(1/2/3): 59-88.
[9] Popp B N, Anderson T F, Sandberg P A. Brachiopods as indicators of original isotopic compositions in some Paleozoic limestones[J]. Bulletin of the Geological Society of America, 1986, 97(10): 1262-1269.
[10] van Geldern R, Joachimski M M, Day J, et al. Carbon, oxygen and strontium isotope records of Devonian brachiopod shell calcite[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 240(1/2): 47-67.
[11] Lowenstam H A. Mineralogy, O18/O16 ratios, and strontium and magnesium contents of recent and fossil Brachiopods and their bearing on the history of the oceans[J]. The Journal of Geology, 1961, 69(3): 241-260.
[12] Veizer J, Fritz P, Jones B. Geochemistry of brachiopods: Oxygen and carbon isotopic records of Paleozoic oceans[J]. Geochimica et Cosmochimica Acta, 1986, 50(8): 1679-1696.
[13] Wadleigh M A, Veizer J.18O/16O and 13C/12C in lower Paleozoic articulate brachiopods: Implications for the isotopic composition of seawater[J]. Geochimica et Cosmochimica Acta, 1992, 56(1): 431-443.
[14] Mii H S, Grossman E L. Late Pennsylvanian seasonality reflected in the 18O and elemental composition of a brachiopod shell[J]. Geology, 1994, 22(7): 661-664.
[15] Qing Hairuo, Veizer J. Oxygen and carbon isotopic composition of Ordovician brachiopods: Implications for coeval seawater[J]. Geochimica et Cosmochimica Acta, 1994, 58(20): 4429-4442.
[16] Carpenter S J, Lohmann K C. δ18O and δ13C values of modern brachiopod shells[J]. Geochimica et Cosmochimica Acta, 1995, 59(18): 3749-3764.
[17] 李心清,万国江,周会. 腕足化石壳体氧,碳同位素生命效应问题研究[J]. 自然科学进展,2000,10(5):435-442.[Li Xinqing, Wan Guojiang, Zhou Hui. The study of vital effect of oxygen, carbon isotope on brachiopod fossil shells[J]. Progress of Natural Science, 2000, 10(5): 435-442.]
[18] Lee Xinqing, Wan Guojiang. No vital effect on δ18O and δ13C values of fossil brachiopod shells, Middle Devonian of China[J]. Geochimica et Cosmochimica Acta, 2000, 64(15): 2649-2664.
[19] Parkinson D, Curry G B, Cusack M, et al. Shell structure, patterns and trends of oxygen and carbon stable isotopes in modern brachiopod shells[J]. Chemical Geology, 2005, 219(1/4):193-235.
[20] 程红光,李心清,袁洪林,等. 泥盆纪海水的碳,氧同位素变化——来自腕足化石的同位素记录[J]. 地球学报,2009,30(1):79-88.[Cheng Hongguang, Li Xinqing, Yuan Honglin, et al. Carbon and oxygen isotope variations of Devonian seawater: isotopic records from brachiopod fossil shell[J]. Acta Geoscientica Sinica, 2009, 30(1): 79-88.]
[21] Brand U, Veizer J. Chemical diagenesis of a multicomponent carbonate system; 2, Stable isotopes[J]. Journalof Sedimentary Research, 1981, 51(3): 987-997.
[22] 白志强. 泥盆纪华南板块古地理的位置及其漂移[J]. 北京大学学报:自然科学版,1998,34(6):807-812.[Bai Zhiqiang. The paleogeographical position and drift of the southern China Plate in Devonian[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 1998, 34(6): 807-812.]
[23] 中国地质科学院成都地质矿产研究所,中国地质科学院地质研究所. 四川龙门山地区泥盆纪地层古生物及沉积相[M]. 北京:地质出版社,1988:1-158. [Chengdu Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, Institute of Geology, Chinese Academy of Geological Sciences. Devonian Stratigraphy, Paleontology and Sedimentary Facies of Longmenshan, Sichuan[M]. Beijing: Geological Publishing House, 1988: 1-158.]
[24] 黄思静. 川西北甘溪中、上泥盆统海相碳酸盐岩的碳、锶同位素组成及其地质意义[J]. 岩石学报,1993,9(增刊):214-221.[Huang Sijing. Carbon, strontium isotopes of marine carbonate rocks of Middle-Upper Devonian in Ganxi, northwestern Sichuan province and their geological significance[J]. Acta Petrologica Sinica, 1993, 9(Suppl.): 214-221.]
[25] 黄思静,石和,张萌,等. 龙门山泥盆纪锶同位素演化曲线的全球对比及海相地层的定年[J]. 自然科学进展,2002,12 (9):945-952.[Huang Sijing, Shi He, Zhang Meng, et al. Global correlation of strontium isotopic evolutionary curve and marine facies stratigraphic dating of the Devonian in the Longmen mountains areas[J]. Progress in Natural Science, 2002, 12(9): 945-952.]
[26] 卢武长,崔秉荃,杨绍全,等. 甘溪剖面泥盆纪海相碳酸盐岩的同位素地层曲线[J]. 沉积学报,1994,12(3):12-20.[Lu Wuchang, Cui Bingquan, Yang Shaoqnan, et al. Isotope stratigraphic curves of Devonian marine carbonates in Ganqi profile[J]. Acta Sedimentologica Sinica, 1994, 12(3): 12-20.]
[27] Korte C, Jasper T, Kozur H W, et al. δ18O and δ13C of Permian brachiopods: A record of seawater evolution and continental glaciation[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 224(4): 333-351.
[28] Korte C, Kozur H W, Veizer J. δ13C and δ18O values of Triassic brachiopods and carbonate rocks as proxies for coeval seawater and palaeotemperature[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 226(3/4): 287-306.
[29] Morrison J O, Brand U. Geochemistry of recent marine invertebrates[J]. Geoscience Canada, 1986, 13(4): 237-254.
[30] Brand U. Global climatic changes during the Devonian-Mississippian: Stable isotope biogeochemistry of brachiopods[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1989, 75(4): 311-329.
[31] Denison R E, Koepnick R B, Fletcher A, et al. Criteria for the retention of original seawater87Sr/ 86Sr in ancient shelf limestones[J]. Chemical Geology, 1994, 112(1/2): 131-143.
[32] 桑树勋,郑永飞,张华,等. 徐州地区下古生界碳酸盐岩的碳、氧同位素研究[J]. 岩石学报,2004,20(3):707-716.[Sang Shuxun. Zheng Yongfei, Zhang Hua, et al. Researches on carbon and oxygen stable isotopes of Lower Paleozoic carbonates in Xuzhou area[J]. Acta Petrologica Sinica, 2004, 20(3): 707-716.]
[33] Samtleben C, Munnecke A, Bickert T, et al. Shell succession, assemblage and species dependent effects on the C/O-isotopic composition of brachiopods -- examples from the Silurian of Gotland[J].Chemical Geology, 2001, 175(1/2):61-107.
[34] Brand U, Brenckle P. Chemostratigraphy of the Mid-Carboniferous boundary global stratotype section and point(GSSP), Bird Spring Formation,Arrow Canyon, Nevada, USA[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 165(3/4): 321-347.
[35] Wenzel B. Differential preservation of primary isotopic signatures in Silurian brachiopods from northern Europe[J]. Journal of Sedimentary Research, 2000, 70(1): 194-209.
[36] Anderson T F, Arthur M A. Stable isotopes of oxygen and carbon and their application to sedimentologic and paleoenvironmental problems[M]// Stable Isotopes in Sedimentary Geology: SEPM, Short Course No.10. Soc Econ Paleontolgists & Mineralogists, 1983: 1-151.
[37] Lea D W. Elemental and isotopic proxies of past ocean temperatures[M]// Elderfield H. The Oceans and Marine Geochemistry. New York: Elsevier, 2003: 365-390.
[38] Brock T D. Life at high temperatures[J]. Science, 1985, 230(4722): 132-138.
[39] Marshall J D. Climatic and oceanographic isotopic signals from the carbonate rock record and their preservation[J]. Geological Magazine, 1992, 129(2): 143-160.
[40] McArthur J M, Howarth R J, Bailey T R. Strontium isotope stratigraphy: LOWESS version 3: Best fit to the marine Sr-isotope curve for 0-509 Ma and accompanying look-up table for deriving numerical age[J]. The Journal of Geology, 2001, 109(2): 155-170.