久米村是十四至十五世紀琉球地方向明國朝貢初期移住那霸的福建人－「閩人三十六姓」－所形成的聚落。久米村人對琉球王國外交、文化、思想、信仰有深遠的影響。本論文以時間為縱軸，以民族集團客觀特徵的姓名、語言、信仰、主觀認同意識為橫軸，探討閩人三十六姓自十四世紀末移住琉球那霸久米村之後至今600年之間，在琉球‧沖繩社會脈絡下改變的過程和因應機制，以及客觀文化特徵與主觀認同意識的相互關係。 論文除「緒論」、「結論」外，本論有六章，第一章「久米村人的形成」，寫久米村人的人來源、社會組織、現況，和久米村的地理位置。第二章「久米村人的職業」，重點在描述久米村人在封貢體系中擔任外交官重要角色的實態。第三章「久米村的姓名」，探討久米村人的命名制度及其因時代所起的變化。第四章「久米村人的語言」，析論久米村人閩南話、漢語官話、琉球語及日語之使用與變遷。第五章「久米村人的宗教信仰」，研析久米村人之祖先崇拜、天妃信仰，以及琉球民間信仰與日本民間信仰對久米村人信仰的影響。三、四、五章並分別就姓名、語言、信仰之客觀的文化特徵，探討其作為久米村人民族邊界的有效性。第六章「久米村人的認定與認同」，敘述琉球王國的身分認定制度，並析論此一制度對久米村人主觀認同的影響。 關鍵詞：沖繩 閩人三十六姓 認定 認同 / Kume Village was initially formed by 36 Fujian clans in the 14th Century when the Ryukyu Islands became one of the tributaries to the Ming Empire of China. Kume Villagers had a great influence on the Ryukyu Kingdom in diplomacy, culture, thought, and belief perspectives. The tenets of this dissertation focus on the development of the people of Kume Village; their careers, the evolution of their languages, their system of assigning names to individuals, and how they related first to China, then later to the Okinawa Kingdom, Japan, and how they were perceived by Okinawans throughout this time. The dissertation consists of six chapters. The first chapter, "The Kume Village", writes where Kume villagers come from originally, its past and present social organization, and the Kume Village geographical position. The second chapter, "The Kume Villagers’ Social Niche", mainly describes the important role Kume villagers play in the tribute system as diplomats. The third chapter, "The Naming of a Kume Villager", discusses the Kume Villagers naming system and its evolution. The fourth chapter "The Kume Villager’s Language” analyzes these 4 languages: Southern Fujian, Chinese Mandarin, Ryukyu Islands, and Japanese as they are imported and integrated by the Kume community. The fifth chapter, "The Kume Villagers Religious Beliefs", analyzes the Kume Villagers worship of ancestors, Tian Fei beliefs, as well as how the Ryukyu Islands folklores and the Japanese folklores influenced Kume Villagers. The third, fourth, and fifth chapters test the validity of name, language, and general belief mores as robust ethnic boundaries. The sixth chapter, "Caste-assignment and Social Identity", narrates the establishment of distinct castes and government relegation of the Kume Villagers into an elite class and analyzes how this policy influenced Kume Villagers. Applying time and several ethnic features as its frames of reference, this dissertation debates in detail the development of the culture of Kume Villagers parallel to and as the result of their interaction with Okinawa society in the last 600 years. Keywords：Okinawa, 36 Fujian clans, Chinese overseas, Identity

RésuméUne série de sondages continentaux (FZ4, FZ5, et SZY) ont été collectés dans la plaine de Fuzhou et dans la montagne de Ningde. Les trois enregistrements ont permis de reconstituer et ainsi de comprendre l'évolution de la végétation ainsi que d'évaluer l'impact de la mousson est-asiatique et les changements du niveau marin sur les environnements du quaternaire récent. Ma thèse donne un aperçu de la végétation passée et des changements paléoclimatiques au cours des 50000 dernières années. Pour les derniers millénaires je me suis aussi intéressé aux activités humaines préhistoriques et leur relation avec les changements de l'environnement local durant l'Holocène. Dans cette thèse, j'ai utilisé une approche multidisciplinaire incluant principalement la palynologie, la sédimentologie, le paléomagnétisme et la micropaléontologie pour reconstituer les environnements passés.L'enregistrement palynologique SZY issu d'une tourbière subalpine couvre les 50000 dernières années en continu. Les diversité de la flore et des changements forestiers au cours des 50 dernières millénaires permettent de reconstituer l'évolution de la mousson régionale dans le sud-est de la Chine. Les changements climatiques estimés par un indice de mousson saisonnier, la température et les précipitations mensuelles ont été quantitativement reconstruits.Les assemblages polliniques pendant la période entre ca. 50 et 30,4 ka cal BP, correspondant au stade isotopique marin (MIS) 3, sont caractérisés par une forte abondance de pollen arboricole, principalement subtropicaux Quercus, Castanopsis/Lithocarpus avec des taxons tempérés de montagne à feuillage caduque tels que Fagus et Alnus et accompagné de quelques conifères mésiques de montagne telles que les Taxodiaceae et Tsuga. Une telle composition de l'écosystème suggère que le MIS 3 était plutôt humide avec une forte mousson d'été. L'insolation d'été élevée peut avoir entraîné une intensification de la mousson au cours de cette période et a donc contribué au maintien d'un tel écosystème subtropical. Une expansion progressive des taxons arborés feuillus, qui a remplacé les taxons subtropicaux à feuillage persistant pendant la période du dernier maximum glaciaire (LGM) (de ca. 30,4 à 11,8 environ cal ka BP), indique que le climat est devenu beaucoup plus frais que lors du MIS 3. Cet intervalle froid se produit entre ca. 21 et 17 cal ka BP lorsque la savane arbustive a augmenté et la forêt de feuillus a diminué rapidement. Cet événement est également marqué par la concentration de pollen qui montre des valeurs faibles au cours du dernier maximum glaciaire. Ceci est probablement lié à un paysage ouvert ou semi-ouvert sous un climat plus sec et plus froid que durant le MIS 3. En comparaison avec les études des isotopes de l'oxygène (δ18O/δ16O) issues de spéléothèmes et ses carottes de glace du Groenland, plusieurs événements climatiques rapides pourraient être reconnues tels que le Dryas récent et l'interstade Bølling-Allerød qui ont marqué la fin de la dernière période glaciaire. Au cours de l'Holocène, la forêt sempervirente est restaurée rapidement. Le groupe arboré à feuillage persistant est devenu plus élevé que celui à feuilles caduques à environ 8000 cal BP. Ceci reflète un renforcement de la mousson d'été. Deux événements rapides semble être enregistré à ca. 8,2 cal ka BP et 5 cal ka BP, probablement causé par des événements de refroidissement au cours de l'Holocène. Dans le tronçon inférieur de la rivière Min, l'étude interdisciplinaire de deux enregistrements révèlent que l'environnement sédimentaire dans la plaine de Fuzhou a connu des cycles de sédimentation à plusieurs reprises au cours de l'Holocène. La première transgression marine dans a eu lieu aux alentours de ca. 9000 cal yr BP, et a atteint son plus haut niveau entre ca. 7000 et 4000 cal yr BP. La granulométrie et l'analyse des diatomées ainsi que les datations 14C AMS permettent de décrire la transgression marine et / AbstractA series of sediment cores (FZ4, FZ5, and SZY) were collected in Fuzhou plain and Ningde mountain area. The three cores, located respectively in the near coast basins and mountains, are well suited for understanding the evolution of vegetation and the impact of the East Asian monsoon and sea level changes on the Quaternary environments. My thesis provides insight into regional palaeovegetation and palaeoclimatic changes over the last 50000 years, as well as an investigation of the prehistoric human activities and their relationship with local environmental change during the Holocene. In this thesis, I have used a multidisciplinary approach including palynology, sedimentology, paleomagnetism and micropaleontology to reconstruct the past environments. The SZY pollen record from a subalpine peat bog covers the past 50,000 years continuously. The diverse flora and forest changes during the last 50 ka indicate regional monsoon evolution in subtropical southeastern China. The climate proxies such as seasonal monsoon index, monthly temperature and precipitation were quantitatively reconstructed.The pollen assemblage during the period ca. 50-30.4 cal ka BP, roughly corresponding to Marine Isotope Stage (MIS) 3, was characterized by high abundance of arboreal pollen, mainly subtropical evergreen Quercus, Castanopsis/Lithocarpus mixed with temperate mountain deciduous broad-leaved trees such as Fagus, Alnus and accompanied with some mountain mesic conifers such as Taxodiaceae and Tsuga. Such ecosystem composition suggests that MIS 3 was rather wet with strong summer monsoon. The high summer insolation may have caused an intensification of the summer monsoon during this period and thus helped maintaining such subtropical ecosystem.A gradual expansion of deciduous broad-leaved taxa which replaced the subtropical evergreen ones during the Last Glacial Maximum (LGM) period (ca. 30.4-11.8 cal ka BP), indicates that climate became much cooler than during MIS 3. The coldest interval occurs during the interval ca. 21-17 cal ka BP, when the shrubby savanna increased and the broadleaved forest rapidly declined. This event is marked also in the pollen concentration which show low values during the LGM. This is probably related to an open or semi-open landscape under a colder and dryer climate than during MIS 3. In comparison with regional oxygen isotope data (δ18O/δ16O) from speleothems and Greenland ice cores, several rapid climate events could be recognized, for instance the Younger Dryas and the Bølling-Allerød interstadial that marked the final stages of the last glacial period. During the Holocene, the evergreen forest restored rapidly. The evergreen pollen group became higher than the deciduous one at around 8000 cal yr BP, reflecting the strengthening of the Summer Monsoon. Two sharp events occurred at ca. 8.2 cal ka BP and ca. 5 cal ka BP, probably caused by cooling events during the Holocene.In the lower reach of Min River, the interdisciplinary study of two cores reveal that the sedimentary environment in Fuzhou Plain experienced several sedimentation cycles during the Holocene. The marine transgression into Fuzhou basin took place in around ca. 9000 cal BP, and reached its highest sea level at 7000-4000 cal BP. Grain-size and diatom analysis and AMS dating allow to depict the marine transgression and reconstruct its timing. Pollen analyses support the warm subtropical climate during the Mid-Holocene with dense forest dominated with evergreen broadleaved taxa. The optimal climate and the formation of marine estuary during the high-stand of the sea level were in favor of the development of the Neolithic culture (mainly Tanshishan Culture between ca. 6800-4500 cal yr BP) where the fishing and hunting were the main economic lifestyles.The sedimentological results show that the retreat of the coastline took place during the late Holocene. This is indicated by a layer of tidal peat dated around ca.1900 cal yr

Thesis (Ph. D.)--University of Hawaii at Manoa, 1982. / Bibliography: leaves 149-157. / Microfiche. / xii, 157 leaves, bound ill. 29 cm

Thesis (M. Phil.)--University of Hong Kong, 1996. / Includes bibliographical references (leaf [249]-266).

Chow Kin On. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2006. / Includes bibliographical references (leaves 106-110). / Abstracts in English and Chinese. / Abstract --- p.i / Acknowledgements --- p.iii / Chapter Chapter One --- Introduction --- p.1 / Chapter 1.1 --- Motivation --- p.1 / Chapter 1.2 --- Contribution --- p.3 / Chapter Chapter Two --- Overview China's Administration System --- p.6 / Chapter 2.1 --- Development of China's System of Administrative Jurisdictions --- p.6 / Chapter 2.2 --- Administration System of Zhejiang --- p.15 / Chapter 2.3 --- Administration System of Fujian --- p.19 / Chapter Chapter Three --- Literature Review --- p.23 / Chapter 3.1 --- Advantages and Disadvantages of Province- Administering-County (PAC) System --- p.23 / Chapter 3.2 --- Literature on Prefecture-Level-City-Administering-County (CAC) System --- p.26 / Chapter 3.3 --- Literature on Economic Growth --- p.30 / Chapter Chapter Four --- Methodology --- p.34 / Chapter 4.1 --- Growth Regression Model and Approaches --- p.34 / Chapter 4.2 --- Explanatory Variables --- p.39 / Chapter Chapter Five --- Estimation Results --- p.47 / Chapter 5.1 --- Estimation Results --- p.47 / Chapter 5.2 --- Summary and Interpretation of Estimation Results --- p.53 / Chapter Chapter Six --- Policy Implications and Conclusion --- p.58 / Chapter 6.1 --- Summary of Major Findings --- p.58 / Chapter 6.2 --- Policy Implications --- p.59 / Chapter 6.3 --- Limitation and Possible Extensions --- p.63 / Appendix --- p.65 / Reference --- p.106

Tam, Su San. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2009. / Includes bibliographical references (leaves 144-147). / Abstracts in English and Chinese; includes Chinese characters. / ABSTRACT --- p.I / ACKNOWLEDGEMENTS --- p.IV / TABLE OF CONTENTS --- p.VI / Chapter CHAPTER 1 --- INTRODUCTION --- p.1 / Chapter 1.1 --- Background of the Problem and Purpose of the Study --- p.1 / Chapter 1.2 --- Research Questions and Significance of the Study --- p.3 / Chapter 1.3 --- Scope of the Study --- p.3 / Chapter 1.4 --- Thesis Organization --- p.4 / Chapter CHAPTER 2 --- DATA OF FOUR SOUTHERN MIN DIALECTS --- p.1 / Chapter 2.1 --- Preamble --- p.1 / Chapter 2.2 --- Basic Data of the four sub-dialects --- p.2 / Chapter 2.2.1 --- Xiamen Dialect --- p.2 / Chapter 2.2.1.1 --- Xiamen Onsets --- p.3 / Chapter 2.2.1.2 --- Xiamen Rimes --- p.4 / Chapter 2.2.1.3 --- Xiamen Tones --- p.7 / Chapter 2.2.1.4 --- Xiamen Syllables --- p.7 / Chapter 2.2.2 --- Quanzhou Dialect --- p.8 / Chapter 2.2.2.1 --- Quanzhou Onsets --- p.8 / Chapter 2.2.2.2 --- Quanzhou Rimes --- p.9 / Chapter 2.2.2.3 --- Quanzhou Tones --- p.11 / Chapter 2.2.2.4 --- Quanzhou Syllables --- p.12 / Chapter 2.2.3 --- Zhangping Dialect --- p.13 / Chapter 2.2.3.1 --- Zhangping Onsets --- p.13 / Chapter 2.2.3.2 --- Zhangping Rimes --- p.14 / Chapter 2.2.3.3 --- Zhangping Tones --- p.16 / Chapter 2.2.3.4 --- Zhangping Syllables --- p.16 / Chapter 2.2.4 --- Shantou Dialect --- p.17 / Chapter 2.2.4.1 --- Shantou Onsets --- p.17 / Chapter 2.2.4.2 --- Shantou Rimes --- p.19 / Chapter 2.2.4.3 --- Shantou Tones --- p.21 / Chapter 2.2.4.4 --- Shantou Syllables --- p.21 / Chapter 2.3 --- Co-occurrence Patterns --- p.22 / Chapter 2.3.1 --- On Labial Co-occurrence --- p.22 / Chapter 2.3.1.1 --- Xiamen Labial Co-occurrence --- p.23 / Chapter 2.3.1.2 --- Quanzhou Labial Co-occurrence --- p.24 / Chapter 2.3.1.3 --- Zhangping Labial Co-occurrence --- p.26 / Chapter 2.3.1.4 --- Shantou Labial Co-occurrence --- p.27 / Chapter 2.3.1.5 --- Southern Min Labial Co-occurrence: A Summary --- p.28 / Chapter 2.3.2 --- On nasalization --- p.29 / Chapter 2.3.2.1 --- Xiamen Nasalization --- p.30 / Chapter 2.3.2.2 --- Quanzhou Nasalization --- p.32 / Chapter 2.3.2.3 --- Zhangping Nasalization --- p.35 / Chapter 2.3.2.4 --- Shantou Nasalization --- p.37 / Chapter 2.3.2.5 --- Southern Min Nasality: A Summary --- p.40 / Chapter 2.4 --- Generalizing the Southern Min Phonotactic Observations --- p.41 / Chapter CHAPTER 3 --- PREVIOUS STUDIES ON CHINESE/MIN PHONOTACTICS --- p.44 / Chapter 3.1 --- Autosegmental Phonology --- p.44 / Chapter 3.1.1 --- Obligatory Contour Principle (OCP) --- p.46 / Chapter 3.1.1.2 --- OCP and Labial Co-Occurrence in Chinese Syllables --- p.49 / Chapter 3.1.1.3 --- Application of OCP in Southern Min Dialects --- p.54 / Chapter 3.1.2 --- Syllable Theory in Chinese and Southern Min --- p.58 / Chapter 3.1.3 --- Nasality in Southern Min --- p.65 / Chapter 3.1.3.1 --- Nasal Consonants --- p.65 / Chapter 3.1.3.2 --- Nasalized Vowels --- p.67 / Chapter 3.1.3.3 --- Derivation of Nasality in Southern Min --- p.68 / Chapter 3.1.4 --- Inadequacies of Autosegmental Framework --- p.76 / Chapter 3.2 --- Optimality Theory (OT) --- p.79 / Chapter 3.2.1 --- Revisiting OCP in OT --- p.83 / Chapter 3.2.2 --- Nasalization in OT --- p.89 / Chapter CHAPTER 4 --- AN OPTIMALITY ANALYSIS OF THE SOUTHERN MIN PHONOTACTICS --- p.93 / Chapter 4.1 --- On labial co-occurrence --- p.93 / Chapter 4.2 --- On nasalization --- p.103 / Chapter 4.3 --- Summary: a Southern Min 'Typology' --- p.116 / Chapter CHAPTER 5 --- CONCLUSION --- p.118 / Chapter 5.1 --- Conclusion --- p.118 / Chapter 5.2 --- Residual Issues and Future Research --- p.119 / APPENDICES --- p.121 / Appendix A ´ؤ Xiamen Syllable Chart --- p.122 / Appendix B - Quanzhou Syllable Chart --- p.128 / Appendix C 一 Zhangping Syllable Chart --- p.134 / Appendix D - Shantou Syllable Chart --- p.138 / REFERENCES --- p.144

近二十年來，中共對台資企業的政策演變相當複雜，從政策形成、制定、執行、評估與修訂觀看，實際上已走過一次或多次的政策循環，也歷經不同的環境、機構、決策者與政策學習。瞭解這長期的演變具有相當研究價值。但這政策研究不能只專注於負責政策制定的中央部門，而疏略實際執行地方政府的重要角色。因此，將政策佈局與實踐落腳到特定的地區與地點，可從中獲得深層的政策真相，甚或背離。 在大陸各省中，福建與台灣隔海相望關係最為密切，歸納有地緣、血緣、史緣、香火、物緣、俗緣等六大親密關係。選擇福建省作為個案研究對象，頗能突出這人文、歷史特點。從實際出發亦較之對大陸其它省份更兼具現實意義。換言之，閩台間具有這種相同或相近的人文、歷史與族際文化關係，有著長期穩定性，經得起任何環境變遷衝擊，而尋得認同與所謂「回歸」作用。而北京在規劃福建對台開放戰略的針對性，不會放過這諸因素在各方面的特殊作用。 隨兩岸關係進展，大陸改革開放的擴大與深化，閩台交往日漸頻繁，研究福建台資政策更加引起我們重視。本文結合歷史研究法與系統理論的研究架構，針對福建個案的演變進行分析，並提出一些規範性思考供參。 本文第一個研究主題，分析影響福建台資政策的長期與短期環境變數。研究發現福建台資政策發展過程與實踐與大陸政經情勢及兩岸關係發展進程密切相關，並確實體現其特殊對台關係與優勢。 本文第二個研究主題，是在探討決策者或參與者對福建台資政策之影響，並以「省領導層」為出發點，向上溯及與中共中央領導層的互動，向下伸延與所屬地方執行階層彼此關聯，針對決策互動與發展過程進行研究。研究發現政策環境、政策信仰、派系、領導特質等因素影響台資政策的發展。從長期來看，環境決定政策方向，其餘因素左右政策速度與範圍。 本文第三個研究主題，是探討福建台資政策的產出。研究發現台資政策的發展相當複雜，在福建的政策地位與重要性因時而異，從政策方向、速度、範圍、形式與群聚性，觀察政策的長期演變，發現細部政策行走軌跡並非是直線發展，它的真實面貌停停走走較接近曲折前進，並呈現階段性的盤旋。 本文第四個研究主題，剖析福建與北京在台資政策的互動與博奕關係。研究發現，其一：福建相當擔心兩岸政治角力，致北京在該省的軍事行動影響其經濟發展，以及摧毀多年辛苦建立的閩台經濟關係；其二：在涉台經濟議題上，是福建可能向北京採取遊說、蹉商、討價還價，甚至擴張或對抗的領域；其三：在福建發展台資政策的管理、服務等行政措施上，具相當決定權並能發揮政策革新的影響；其四：追求地方經濟利益培育福建滋長異於北京的政策信念，不過經濟力雖把福建推向“閩（華）南經濟圈”的地緣觀，但演進過程福建自身並未斷絕與北京的政治連結關係。 本文第五個討論主題，在說明台資企業在福建投資狀況，研究發現台資占福建利用外資的比例不低，對福建的影響已涵蓋經濟、社經體制等各層面，不只改變部分地市的經建計畫，最重要它提升福建對台工作的優勢地位，並創造向北京提建言、耍周旋的籌碼與機遇。 本文第六個主題，探討政策影響與回饋，從閩台密切經濟交流凸顯兩岸政經互動的意義，發現兩岸經濟聯繫愈密切，相互依存加深，受損性與敏感度增高，在進行政策選擇時顧慮就越多，安全係數也就相應增加。但必須說明，經濟力能降低多少兩岸政治僵局與軍事衝突，以及在何種情況下，它無法發揮調和緩衝的作用，而完全受制於政治因素，仍有待進一步研究。

陳立旺[著] / Thesis (M.A.)--香港中文大學硏究院. / Reprint of manuscript. / Includes bibliographical references (leaves 341-475). / Chen Liwang [zhu] / Thesis (M.A.)--Xianggang Zhong wen da xue yan jiu yuan. / Chapter 第一章 --- 引言 --- p.1 / Chapter 第二章 --- 閩粤地區的自然環境與新石器時代的氣候 --- p.8 / Chapter 第三章 --- 閩粤地區新石器文化分述 --- p.25 / Chapter 壹 --- 文化區劃分 --- p.25 / Chapter 貳 --- 浙南閩北區　 --- p.26 / （附圖一至八十、附表一至九） / Chapter 參　 --- 閩南粤東區 --- p.83 / （附圖一至九十三、附表一至二十一） / Chapter 肆 --- 粤中區 --- p.152 / （附圖一至一十、附表一至九） / Chapter 伍 --- 粤西南及海南島區 --- p.217 / （附圖一至十九、附表一至十一） / Chapter 陸 --- 粤北區　 --- p.256 / （附圖一至二十六、附表一至八） / Chapter 第四章 --- 閩粤地區新石器文化總述 --- p.298 / （附圖一至十） / Chapter 第五章 --- 附論本區及鄰近地區新石器文化之關係 --- p.322 / （附圖一至二十九） / Chapter 附錄一 --- 閩粤地區碳14年代測定數據 --- p.340/341 / Chapter 附錄二 --- 生產工具與生活用具分式分型表　 --- p.340/341 / 書目 --- p.341

朱峰. / "2001年3月" / 論文 (哲學碩士)--香港中文大學, 2001. / 參考文獻 (leaves 150-159) / 附中英文摘要. / "2001 nian 3 yue" / Zhu Feng. / Lun wen (zhe xue shuo shi)--Xianggang Zhong wen da xue, 2001. / Can kao wen xian (leaves 150-159) / Fu Zhong Ying wen zhai yao. / 論文提要 --- p.I / 目錄 --- p.IV / 序言 --- p.VI / Chapter 第一章 --- 導言 --- p.1 / Chapter 一´Ø --- 槪念澄淸 / Chapter 二´Ø --- 研究回顧 / Chapter 第二章 --- 華南女子文理學院的歷史回溯 --- p.12 / Chapter 一´Ø --- 佈道家辦學…程呂底亞時期(1908-1925) / Chapter 二´Ø --- 教育家辦學…盧愛德時期(1925-1927) / Chapter 三´Ø --- 華人治校……王世靜時期(1928-1951) / Chapter 第三章 --- 社會角色的變遷：服務教會與服務社會的互動 --- p.50 / Chapter 一´Ø --- 直接服務教會(1908-1927) / Chapter 二´Ø --- 從服務教會到服務社會(1927´ؤ1949) / Chapter 三´Ø --- “爲人民服務´ح的嘗試(1949一1951) / Chapter 第四章 --- 教育角色的實踐：基督教女子高等教育的特點 --- p.77 / Chapter 一´Ø --- 宗教教育與愛國主義 / Chapter 二´Ø --- 女權辯論與家政專業 / Chapter 三´Ø --- 校友統計與個案分析 / Chapter 第五章 --- 性別角色的追尋：與福建協和大學的合倂爭論 --- p.114 / Chapter 一´Ø --- 合倂爭論的困擾 / Chapter 二´Ø --- 合倂爭論的分析 / Chapter 三´Ø --- 合倂爭論的意義 / 結語 --- p.133 / 參考書目 / 附錄一 ：2000年度問卷調˘¬表和基本數據 / 附錄二：華南女子文理學院學生畢業論文題目(部分） / 附錄三：華南女子文理學院教職員工履歷表 / 附錄四：金陵女院與華南女院各項統計數字比照(1934年） / 附錄五：華南女子文理學院財政收入比例變化表 / 附錄五：中外人名漢/英對照表

Mei Qing. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2000. / Includes bibliographical references (leaves 123-138). / Abstracts in English and Chinese. / Chapter Chapter 1. --- Introduction --- p.1 / Chapter 1.1 --- Literature Review --- p.4 / Chapter 1.2 --- Methodology --- p.8 / Chapter Chapter 2. --- Seeking A New World --- p.16 / Chapter 2.1 --- Historical Context --- p.16 / Chapter 2.2 --- "Geographical and Cultural Context of Malacca, Penang and Singapore" --- p.22 / Chapter 2.3 --- The Development of Chinese Temples and Huiguans in the Settlements --- p.33 / Chapter Chapter 3. --- Between Two Worlds: Temple Studies --- p.40 / Chapter 3.1 --- Chinese Belief Structure --- p.40 / Chapter 3.2 --- Prototype of Temples in Fujian --- p.49 / Chapter 3.3 --- Cheng Hoon Teng in Malacca … --- p.52 / Chapter 3.4 --- Guang Fu Gong and Tian Fu Gong --- p.75 / Chapter 3.5 --- Summary … --- p.88 / Chapter Chapter 4. --- Between Two Worlds: Huiguan Studies --- p.92 / Chapter 4.1 --- Origin of Huiguans in China --- p.93 / Chapter 4.2 --- Chinese Huiguans in the Straits --- p.97 / "Conclusion: Temple, Huiguan, and Identity" --- p.121 / Bibliography