浮游有孔虫标准化壳体重量测试方法及在西太平洋的应用

安佰正; 李铁刚; 孙晗杰; 熊志方; 常凤鸣

doi:10.3799/dqkx.2015.072

浮游有孔虫标准化壳体重量测试方法及在西太平洋的应用

doi: 10.3799/dqkx.2015.072

安佰正^{1, 2,},
李铁刚^1, ,,
孙晗杰¹,
熊志方¹,
常凤鸣¹

1.
中国科学院海洋研究所，中国科学院海洋地质与环境重点实验室，山东青岛 266071
2.
中国科学院大学，北京 100049

基金项目:

中国科学院战略性先导科技专项项目 XDA10010305

国家海洋局专项项目 GASI-04-01-02

国家自然科学基金项目 41230959

国家自然科学基金项目 41206044

详细信息

作者简介:
安佰正(1984-)，男，博士研究生，主要从事古海洋学、浮游有孔虫研究.E-mail: an_baizheng@126.com

通讯作者:
李铁刚，E-mail: tgli@qdio.ac.cn

中图分类号: P736.2
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- 被引次数: 0
出版历程
- 收稿日期: 2014-10-15
- 刊出日期: 2015-05-15

Application of Planktonic Foraminifera Size-Normalized Shell Weight in the Western Pacific

1.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao266071, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

摘要

摘要: 使用标准化壳体重量法和传统壳体重量法分别对中国南海(South China Sea，简称SCS)站表层沉积物和MD06-3052岩心沉积物样品进行了测试，获得了浮游有孔虫种属Globigerinoides ruber(G. ruber)的标准化壳体重量和传统壳体重量.通过对SCS站表层沉积物中G. ruber标准化壳体重量与传统壳体重量的比较，认为在该海域使用标准化壳体重量替代性指标能够更好的排除壳体粒径的干扰.通过对MD06-3052岩心中G. ruber标准化壳体重量与南极Vostok冰心的CO₂浓度(pCO₂)曲线进行对比，认为标准化壳体重量方法能够较好的反映出表层海水[CO₃^2-]的变化.标准化壳体重量方法快速简便，指示性好，在探讨晚更新世以来表层海水在全球碳循环的重要作用中，是一个很有潜力的指标.
- 标准化壳体重量 /
- 浮游有孔虫 /
- 碳酸盐 /
- 碳循环 /
- 西太平洋 /
- 海洋地质
Abstract: Planktonic foraminifera Globigerinoides ruber (G. ruber) shell weight of sediment samples from South China Sea (SCS) located in the South China Sea and MD06-3052 located in the western Pacific are tested using size-normalized shell weight method and traditional shell weight method. In comparison with traditional shell weight method, SCS data indicate that the size-normalized shell weight method for G. ruber can significantly reduce the influence of test size on foraminifera shell weight in the study area. Comparing the variation curves of CO₂ concentration (pCO₂) recorded in Vostok ice core, MD06-3052 G. ruber data show that size-normalized shell weight can indicate the change of sea surface water [CO₃^2-] more effectively. The size-normalized shell weight method provides a reliable and rapid proxy for the weight analyses in the paleoceanographic study, and a potential proxy in studying the influence of surface sea water in global carbon cycle since Late Pleistocene.
- size-normalized shell weight /
- planktonic foraminifera /
- carbonate /
- carbon cycle /
- the western Pacific /
- marine geology

HTML全文

图 1 浮游有孔虫标准化壳体重量方案流程

Fig. 1. Process of planktonic foraminifera size-normalized shell weight method

下载: 全尺寸图片幻灯片

图 2 ImageJ软件对图像进行锐化和寻找边缘

Fig. 2. Sharpen and find edges using ImageJ

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图 3 使用ImageJ软件获得有孔虫的最小外切圆

Fig. 3. Get minimum excircle of foraminifera shell using ImageJ

下载: 全尺寸图片幻灯片

图 4 SCS站浮游有孔虫G. ruber传统壳体重量方法与标准化壳体重量方法的对比

传统壳体重量(红色)与壳体直径的相关系数R=0.840；标准化壳体重量(蓝色)与壳体直径的相关系数R=0.299

Fig. 4. Traditional shell weight method and size-normalized shell weight method for G. ruber in SCS

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图 5 SCS站表层沉积物浮游有孔虫G. ruber壳体重量与样本中壳体总数的关系

Fig. 5. Relationship of shell weight and sum of G. ruber of surface sediments in SCS

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图 6 MD06-3052岩心浮游有孔虫G. ruber传统壳体重量方法(a)与标准化壳体重量方法(b)的对比

图 6a中相关系数R=0.742；图 6b中相关系数R=0.451

Fig. 6. Traditional shell weight method (a) and size-normalized shell weight method (b) for G. ruber in MD06-3052

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图 7 MD06-3052岩心浮游有孔虫G. ruber标准化壳体重量(蓝色曲线)与南极冰心大气pCO₂变化曲线(粉色曲线)对比

Fig. 7. Size-normalized shell weight of planktonic foraminifera G. ruber in MD06-3052(blue line) and Vostok pCO₂ record (pink line)

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表 1 MD06-3052岩心浮游有孔虫G. ruber标准化壳体重量及传统壳体重量

Table 1. Size-normalized shell weight and traditional shell weight of planktonic foraminifera G. ruber from MD06-3052

样品号	样品层位(cm)	年代(ka BP)	壳体数量(个)	传统壳体重量(μg)	标准化壳体重量(μg)
1	54~56	3.34	6	7.83	8.84
2	182~184	10.58	11	8.45	10.60
3	238~240	14.45	6	12.50	12.97
4	278~280	19.00	13	14.85	14.07
5	342~344	24.41	11	13.00	13.23
6	390~392	28.00	9	12.89	12.97
7	430~432	30.86	6	12.33	12.73
8	486~488	34.87	11	12.64	13.02
9	574~576	41.17	11	13.64	13.84
10	646~648	46.25	11	11.27	12.46
11	678~680	48.32	8	10.00	11.06

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参考文献(48)

Abràmoff, M.D., Magalhães, P.J., Ram, S.J., 2004. Image Processing with Image. J. Biophotonics International, 11(7): 36-42.
Aldridge, D., Beer, C.J., Purdie, D.A., 2012. Calcification in the Planktonic Foraminifera Globigerina bulloides Linked to Phosphate Concentrations in Surface Waters of the North Atlantic Ocean. Biogeosciences, 9(5): 1725-1739. doi: 10.5194/bg-9-1725-2012
Anderson, D.M., Archer, D., 2002. Glacial-Interglacial Stability of Ocean pH Inferred from Foraminifer Dissolution Rates. Nature, 416(6876): 70-73. doi: 10.1038/416070a
Barker, S., Elderfield, H., 2002. Foraminiferal Calcification Response to Glacial-Interglacial Changes in Atmospheric CO₂. Science, 297(5582): 833-836. doi: 10.1126/science.1072815
Beer, C.J., Schiebel, R., Wilson, P.A., 2010. Technical Note: On Methodologies for Determining the Size-Normalised Weight of Planktic Foraminifera. Biogeosciences, 7(7): 2193-2198. doi: 10.5194/bg-7-2193-2010
Bijma, J., Hönisch, B., Zeebe, R.E., 2002. Impact of the Ocean Carbonate Chemistry on Living Foraminiferal Shell Weight: Comment on "Carbonate Ion Concentration in Glacial-Age Deep Waters of the Caribbean Sea" by W.S. Broecker and E. Clark. Geochemistry, Geophysics, Geosystems, 3(11): 1064. doi: 10.1029/2002GC000388
Bijma, J., Spero, H.J., Lea, D.W., 1999. Reassessing Foraminiferal Stable Isotope Geochemistry: Impact of the Oceanic Carbonate System (Experimental Results). In: Fischer, G., Wefer, G., eds., Use of Proxies in Paleoceanography: Examples from the South Atlantic. Springer, Berlin, 489-512.
Broecker, W.S., Clark, E., 2001a. Glacial-to-Holocene Redistribution of Carbonate Ion in the Deep Sea. Science, 294(5549): 2152-2155. doi: 10.1126/science.1064171
Broecker, W.S., Clark, E., 2001b. An Evaluation of Lohmann's Foraminifera Weight Dissolution Index. Paleoceanography, 16(5): 531-534. doi: 10.1029/2000PA000600
Broecker, W.S., Clark, E., 2004. Shell Weights from the South Atlantic. Geochemistry, Geophysics, Geosystems, 5(3): Q03003. doi: 10.1029/2003GC000625
Chen, R.H., Meng, Y., Li, B.H., et al., 1999. Variations in the Lysocline of Carbonate in the Southern Okinawa Trough during the Last 20000 Years. Marine Geology & Quaternary Geology, 19(1): 25-30(in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/hydzydsjdz199901004
Cooley, S.R., Kite-Powell, H.L., Doney, S.C., 2009. Ocean Acidification's Potential to Alter Global Marine Ecosystem Services. Oceanography, 22(4): 172-181. doi: 10.5670/oceanog.2009.106
Davis, C.V., Badger, M.P.S., Bown, P.R., et al., 2013. Calcification Response to Climate Change in the Pliocene. Biogeosciences Discussions, 10(4): 6839-6860. doi: 10.5194/bgd-10-6839-2013
de Moel, H., Ganssen, G.M., Peeter, F.J.C., et al., 2009. Planktic Foraminiferal Shell Thinning in the Arabian Sea due to Anthropogenic Ocean Acidification. Biogeosciences, 6(9): 1917-1925. doi: 10.5194/bg-6-1917-2009
Doney, S.C., Fabry, V.J., Feely, R.A., et al., 2009. Ocean Acidification: The Other CO₂ Problem. Annu. Rev. Mar. Sci. , 1: 169-192. doi: 10.1146/annurev.marine.010908.163834
Fabry, V.J., Seibel, B.A., Feely, R.A., et al., 2008. Impacts of Ocean Acidification on Marine Fauna and Ecosystem Processes. ICES Journal of Marine Science, 65(3): 414-432. doi: 10.1093/icesjms/fsn048
Fehrenbacher, J., Martin, P., 2011. Western Equatorial Pacific Deep Water Carbonate Chemistry during the Last Glacial Maximum and Deglaciation: Using Planktic Foraminiferal Mg/Ca to Reconstruct Sea Surface Temperature and Seafloor Dissolution. Paleoceanography, 26(2): PA2225. doi: 10.1029/2010PA002035
Hönisch, B., Ridgwell, A., Schmidt, D.N., et al., 2012. The Geological Record of Ocean Acidification. Science, 335(6072): 1058-1063. doi: 10.1126/science.1208277
Hodell, D.A., Charles, C.D., Sierro, F.J., 2001. Late Pleistocene Evolution of the Ocean's Carbonate System. Earth and Planetary Science Letters, 192(2): 109-124. doi: 10.1016/S0012-821X(01)00430-7
Hull, P.M., Norris, R.D., Bralower, T.J., et al., 2011. A Role for Chance in Marine Rcovery from the End-Cretaceous Extinction. Nature Geoscience, 4(12): 856-860. doi: 10.1038/NGEO1302
Logan, C.A., 2010. A Review of Ocean Acidification and America's Response. Bioscience, 60(10): 819-828. doi: 10.1525/bio.2010.60.10.8
Lohmann, G.P., 1995. A Model for Variation in the Chemistry of Planktonic Foraminifera due to Secondary Calcification and Selective Dissolution. Paleoceanography, 10(3): 445-457. doi: 10.1029/95PA00059
Lombard, F., da Rocha, R.E., Bijma, J., et al., 2010. Effect of Carbonate Ion Concentration and Irradiance on Calcification in Planktonic Foraminifera. Biogeosciences, 7(1): 247-255. doi: 10.5194/bg-7-247-2010
Marchitto, T.M., Curry, W.B., Oppo, D.W., 2000. Zinc Concentrations in Benthic Foraminifera Reflect Seawater Chemistry. Paleoceanography, 15(3): 299-306. doi: 10.1029/1999PA000420
Marchitto, T.M., Lynch-Stieglitz, J., Hemming, S.R., 2005. Deep Pacific CaCO₃ Compensation and Glacial-Interglacial Atmospheric CO₂. Earth and Planetary Science Letters, 231(3-4): 317-336. doi: 10.1016/j.epsl.2004.12.024
Marshall, B.J., Thunell, R.C., Henehan, M.J., et al., 2013. Planktonic Foraminiferal Area Density as a Proxy for Carbonate Ion Concentration: A Calibration Study Using the Cariaco Basin Ocean Time Series. Paleoceanography, 28(2): 363-376. doi: 10.1002/palo.20034
Mekik, F., Raterink, L., 2008. Effects of Surface Ocean Conditions on Deep-Sea Calcite Dissolution Proxies in the Tropical Pacific. Paleoceanography, 23(1): PA1216. doi: 10.1029/2007PA001433
Mekik, F.A., Anderson, R.F., Loubere, P., et al., 2012. The Mystery of the Missing Deglacial Carbonate Preservation Maximum. Quaternary Science Reviews, 39: 60-72. doi: 10.1016/j.quascirev.2012.01.024
Moy, A.D., Howard, W.R., Bray, S.G., et al., 2009. Reduced Calcification in Modern Southern Ocean Planktonic Foraminifera. Nature Geoscience, 2(4): 276-280. doi: 10.1038/NGEO460
Naik, S.S., Naidu, P.D., 2007. Calcite Dissolution along a Transect in the Western Tropical Indian Ocean: A Multiproxy Approach. Geochemistry, Geophysics, Geosystems, 8(8): Q08009. doi: 10.1029/2007GC001615
Naik, S.S., Naidu, P.D., Govil, P., et al., 2010. Relationship between Weights of Planktonic Foraminifer Shell and Surface Water CO₃^2- Concentration during the Holocene and Last Glacial Period. Marine Geology, 275(1-4): 278-282. doi: 10.1016/j.margeo.2010.05.004
Orr, J.C., Fabry, V.J., Aumont, O., et al., 2005. Anthropogenic Ocean Acidification over the Twenty-First Century and Its Impact on Calcifying Organisms. Nature, 437(7059): 681-686. doi: 10.1038/nature04095
Palmer, M.R., Pearson, P.N., 2003. A 23 000-Year Record of Surface Water pH and pCO₂ in the Western Equatorial Pacific Ocean. Science, 300(5618): 480-482. doi: 10.1126/science.1080796
Petit, J.R., Jouzel, J., Raynaud, D., et al., 1999. Climate and Atmospheric History of the Past 420 000 Years from the Vostok Ice Core, Antarctica. Nature, 399(6735): 429-436. doi: 10.1038/20859
Qiu, X.H., Li, T.G., Chang, F.M., et al., 2012. Turbidite Deposition Record and Its Mechanism since 150 ka BP in Western Philippine Sea. Marine Geology & Quaternary Geology, 32(4): 157-163(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ201204026.htm
Regenberg, M., Schröder, J.F., Jonas, A.S., et al., 2013. Weight Loss and Elimination of Planktonic Foraminiferal Tests in a Dissolution Experiment. Journal of Foraminiferal Research, 43(4): 406-414. doi: 10.2113/gsjfr.43.4.406
Russell, A.D., Hönisch, B., Spero, H.J., et al., 2004. Effects of Seawater Carbonate Ion Concentration and Temperature on Shell U, Mg, and Sr in Cultured Planktonic Foraminifera. Geochimica et Cosmochimica Acta, 68(21): 4347-4361. doi: 10.1016/j.gca.2004.03.013
Spero, H.J., Bijma, J., Lea, D.W., et al., 1997. Effect of Seawater Carbonate Concentration on Foraminiferal Carbon and Oxygen Isotopes. Nature, 390(6659): 497-500. doi: 10.1038/37333
Solomon, S., Qin, D.H., Manning, M., et al., 2007. Climate Change 2007: The Physical Science Basis: Working Group I Contribution to the Fourth Assessment Report of the IPCC. Cambridge University Press, New York.
Wang, P.X., Min, Q.B., Bian, Y.H., et al., 1986. Planktonic Foraminifera in the Continental Slope of the Northern South China Sea during the Last 130 000 Years and Their Paleo-Oceanographic Implications. Acta Geologica Sinica, 60(3): 215-225(in Chinese with English abstract). doi: 10.1111/j.1755-6724.1986.mp60003001.x/abstract
Xu, J., Huang, B.Q., Chen, R.H., et al., 2001. Distribution of Foraminifera in Surface Sediments of Northeastern South China Sea and Its Environmental Implications. Journal of Tropical Oceanography, 20(4): 6-13(in Chinese with English abstract). http://europepmc.org/abstract/cba/354100
Zeebe, R.E., 2012. History of Seawater Carbonate Chemistry, Atmospheric CO₂, and Ocean Acidification. Annual Review of Earth and Planetary Sciences, 40: 141-165. doi: 10.1146/annurev-earth-042711-105521
Zhang, L.L., Chen, M.H., Chen, Z., et al., 2010. Distribution of Calcium Carbonate and Its Controlling Factors in Surface Sediments of the South China Sea. Earth Science—Journal of China University of Geosciences, 35(6): 891-898(in Chinese with English abstract). doi: 10.3799/dqkx.2010.104
陈荣华, 孟翊, 李保华, 等, 1999. 冲绳海槽南部两万年来碳酸盐溶跃面的变迁. 海洋地质与第四纪地质, 19(1): 25-30. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ901.003.htm
仇晓华, 李铁刚, 常凤鸣, 等, 2012. 西菲律宾海15万年以来的浊流沉积及其成因. 海洋地质与第四纪地质, 32(4): 157-163. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201204026.htm
汪品先, 闵秋宝, 卞云华, 等, 1986.130 000年来南海北部陆坡的浮游有孔虫及其古海洋学意义. 地质学报, 60(3): 215-225. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198603000.htm
徐建, 黄宝琦, 陈荣华, 等, 2001. 南海东北部表层沉积中有孔虫的分布及其环境意义. 热带海洋学报, 20(4): 6-13. https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY200104001.htm
张兰兰, 陈木宏, 陈忠, 等, 2010. 南海表层沉积物中的碳酸钙含量分布及其影响因素. 地球科学——中国地质大学学报, 35(6): 891-898. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201006002.htm