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Search Symbol (Half-width) Description of Search Symbols
Space "AND" indicates the intertwining of key terms used in a search
Double Quotation Marks ("") ( " " ) Double quotation marks indicate the beginning and end of a phrase, and the search will only include terms that appear in the same order of those within the quotations. Example: "image process" : " image process "
? Indicates a variable letter. Entering two ? will indicate two variable letters, and so on. Example: "Appl?", search results will yield apple, apply… e , appl y … ( (often used to English word searches) )
* Indicates an unlimited number of variable letters to follow, from 1~n. Example: Enter "appl*", search results will yield apple, apples, apply, applied, application…(often used in English word searches) e , appl es , appl y , appl ied , appl ication … ( (often used to English word searches) )

Boolean logic combinations of key words is a skill used to expand or refine search parameters.
(1) AND (1) AND: Refines search parameters
(2) OR (2) OR: Expands search parameters (3) NOT: Excludes irrelevant parameters


DOI stands for Digital Object Identifier ( D igital O bject I dentifier ) ,
and is the unique identifier for objects on the internet. It can be used to create persistent link and to cite articles.

Using DOI as a persistent link

To create a persistent link, add「」 「 」 before a DOI.
For instance, if the DOI of an article is 10.5297/ser.1201.002 , you can link persistently to the article by entering the following link in your browser: 10.5297/ser.1201.002
The DOI link will always direct you to the most updated article page no matter how the publisher changes the document's position, avoiding errors when engaging in important research.

Cite a document with DOI

When citing references, you should also cite the DOI if the article has one. If your citation guideline does not include DOIs, you may cite the DOI link.

DOIs allow accurate citations, improve academic contents connections, and allow users to gain better experience across different platforms. Currently, there are more than 70 million DOIs registered for academic contents. If you want to understand more about DOI, please visit airiti DOI ) 。

Abstract 〈TOP〉
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Reference ( 20 ) 〈TOP〉
  1. 呂佳蓉 (2006), 利用磁場式感應耦合電漿質譜儀精確測量碳酸鹽類之鎂鈣及鍶鈣比值, 碩士論文, 10-32 pp, 台灣大學. 莊智凱 (2008), 西赤道太平洋所羅門海ODP1115B站位上部上新統至更新統鈣質超微化石生物地層硏究, 碩士論文, 台灣大學. 陳貞吟 (2006), 以「異時發生」觀點探討浮游有孔蟲Globigerinoides fistulosus的絕滅, 學士論文, 台灣大學. Anand, P., Elderfield, H., and Conte, M. H. (2003). Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2). Barker, S., Greaves, M., and Elderfield, H. (2003). A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry. Geochemistry Geophysics Geosystems, 4. Bé, A. W. H. (1980). Gametogenic Calcification in a Spinose Planktonic Foraminifer, Globigerinoides sacculifer (Brady). Marine Micropaleontology, 5(3), 283-310. Bé, A. W. H., Anderson, O. R., Faber, W. W., and Caron, D. A. (1983). Sequence of Morphological and Cytoplasmic Changes During Gametogenesis in the Planktonic Foraminifer Globigerinoides sacculifer (Brady). Micropaleontology, 29(3), 310-325. Bé, A. W. H., Caron, D. A., and Anderson, O. R. (1981). Effects of Feeding Frequency on Life Processes of the Planktonic Foraminifer Globigerinoides-Sacculifer in Laboratory Culture. Journal of the Marine Biological Association of the United Kingdom, 61(1), 257-277.
  2. Bemis, B. E., Spero, H. J., Bijma, J., and Lea, D. W. (1998). Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations. Paleoceanography, 13(2), 150-160.
  3. McNown, J. S. (1950). Effects of particle shape on settling velocity at low. Nanking: Scientific Book Company.
  4. Thunell, R., Tappa, E., Pride, C., and Kincaid, E. (1999). Sea-surface temperature anomalies associated with the 1997-1998 El Nino recorded in the oxygen isotope
  5. Berger, W. H. (1969). Kummerform Foraminifera as clues to oceanic environments. Amer. Ass. Pet. Geol., Bull., 53, 706. Berger, W. H., and Piper, D. J. W. (1972). Planktonic Foraminifera - Differential Settling, Dissolution, and Redeposition. Limnology and Oceanography, 17(2), 275. Berger, W. H., Bickert, T., Schmidt, H., and Wefer, G. (1993). Quaternary Oxygen Isotope Record Of Pelagic Foraminifers:Site 806, Ontong Java Plateau: Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 130. Berger, W. H., Killingley, J. S., and Vincent, E. (1978). Stable Isotopes in Deep-Sea Carbonates - Box Core Erdc-92, West Equatorial Pacific. Oceanologica Acta, 1(2), 203-216. Berggren, W. A., Kent, D. V., and Van Couvering, J. A. (1985). The Neogene, pt.2, Neogene geochronology and chronostratigraphy (Vol. Neogene geochronology and chronostratigraphy). London: Geol. Soc. London Spec. Pap.,. Bijma, J., and Hemleben, C. (1994). Population-Dynamics of the Planktic Foraminifer Globigerinoides sacculifer (Brady) from the Central Red-Sea. Deep-Sea Research Part I-Oceanographic Research Papers, 41(3), 485-510. Bijma, J., Faber, W. W., and Hemleben, C. (1990). Temperature and Salinity Limits for Growth and Survival of Some Planktonic Foraminifers in Laboratory Cultures. Journal of Foraminiferal Research, 20(2), 95-116. Bostock, H. C., Opdyke, B. N., Gagan, M. K., and Fifield, L. K. (2004). Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation. Paleoceanography, 19(4).
Times Cited (2) 〈TOP〉
  1. 莊智凱(2008)。西赤道太平洋所羅門海ODP1115B站位上部上新統至更新統鈣質超微化石生物地層硏究。臺灣大學地質科學研究所學位論文。2008。1-62。 
  2. 柯惠親(2007)。西赤道太平洋所羅門海ODP 1115B岩芯之氧碳同位素地層記錄。臺灣師範大學地球科學系學位論文。2007。1-85。
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