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| 1 | 末次冰消期以来巽他陆架高分辨率的孢粉记录显示文摘根据南海南部巽他陆坡上的柱状剖面SONNE18287的高分辨率的孢粉记录,重建16500a以来该地区植被和气候的变化历史.研究结果发现冰消期的16.5~13.9kaBP期间,植被是以低山雨林和低地雨林为主,蕨类的低含量及大量的低山雨林成分,反映了较为凉湿的气候.在13.9~10.2kaBP期间,热带低地雨林含量和蕨类植物含量的迅速增长说明了气温升高,而花粉沉积速率的降低反映海平面逐渐上升,研究点与植被源地的距离加大.全新世(10.2kaBP以来),花粉沉积速率进一步降低,仅约为冰消期的1/10,说明巽他陆架已完全被淹没,孢粉主要来自周围岛屿植被.10.2~7kaBP期间的早全新世,低含量的蕨类孢子反映了气温降低;到中全新世(7~3.6kaBP)蕨类孢子含量突然升高,反映了一个相对暖期. | 王晓梅 孙湘君 汪品先 Karl Stattegger | 2007 | 中国科学(D辑)2007，37，1： | 7 |
| 2 | The records of coastline changes reflected by mangroves on the Sunda Shelf since the last 40ka显示文摘This paper presents a 40000-year-long high-resolution mangrove record from sediments of Core 18300,18302 and 18323 on the continental shelf of the southern South China Sea and reconstructs the coast-line changes on Sunda Shelf since the last 40000 years. In the period Marine Isotope 3,the old Sunda Shelf had low sea level,and it was partly exposed. Flourishing vegetations grew on the exposed old land. Mangroves developed along the coastline. On the Last Glacial Maximum,the sea level dropped greatly,coastline moved from inner shelf to outer shelf,the Old Sunda Land exposed further,and the lowering sea level induced the gradual disappearing of mangroves from the inner Sunda Shelf to the outer Sunda Shelf. And pioneer vegetation ferns covered the broadly exposed old land immediately. At the time of the last Deglaciation,sea level rose greatly,the coastline moved to the sea and the Sunda Shelf was drown again. Mangroves were emergent again from outer shelf to inner shelf and developed quickly. | WANG XiaoMei SUN XiangJun WANG PinXian Karl Stattegger | 2008 | Chinese Science Bulletin2008，53，13： | 2 |
| 3 | Rapid flooding of the Sunda Shelf: a late-glacial sea-level record显示文摘 | HANEBUTH Till STATTEGGER Karl GROOTES Pieter | 2000 | Science2000，288，： | 1 |
| 4 | Depositional style and subsidence history of the Turpan Basin(NWChina)显示文摘 | Shao lei Stattegger Karl Li Wenhou | 1999 | Sedimentary Geology1999，128，12： | 1 |
| 5 | Major and trace ele-ments of sDeam sediments from the lowermost Amazon River显示文摘 | Helenice Vital Karl Stattegger | 2000 | Chemical Geology2000，168，： | 1 |
| 6 | Spectrum: spectral analysis of unevenly spaced paleoclimatic time series显示文摘 | Michael Schulz Karl Stattegger | 1997 | Computers and Geosciences1997，，9： | 1 |
| 7 | A high-resolution history of vegetation and climate history on Sunda Shelf since the last glaciation显示文摘This paper presents 16500-year-long high-resolution pollen and spore records from sediments of core 18287 on the continental slope of the southern South China Sea. In the period of 16.5―13.9 ka B.P., the low-mountain rainforest dominated the continental slope of the South China Sea. And in the period of 13.9―10.2 ka B.P., the lowland rainforest and ferns expanded greatly, while the low-mountain rainforest shrank, which indicated a warming at the last deglaciation. Also during this period, the pollen sedi-mentation rates reduced sufficiently. This might imply a rise of the sea level and therefore the sub-mergence of the shelf, resulting in the broadening of the distance between the source area and the slope. After 10.2 ka B.P, decreasing of the fern indicates the early Holocene (10.2―7 ka B.P.) is a cold period, while the increasing of fern marks the rising temperature (7―3.6 ka B.P.). | Karl STATTEGGER | 2007 | Science China Earth Sciences2007，50，1： | 1 |
| 8 | Late Pleistocene forced regressive deposits on the Sunda Shelf(Southeast Asia)显示文摘 | HanebuthTJ J Karl Stattegger Alexander Schimanski | 2003 | Marine Geology2003，，199： | 1 |
| 9 | 显示文摘 | Till J. Hanebuth Karl Stattegger Yoshiki Saito | 2002 | Geo - Marine Letters2002，，2： | 1 |
| 10 | 显示文摘 | Till J. Hanebuth Karl Stattegger Yoshiki Saito | 2002 | Geo - Marine Letters2002，，2： | 1 |
| 11 | Bedrock control on the Assu Incised Valley morphology and sedimentation in the Brazilian Equatorial Shelf显示文摘Assu 切入山谷(AIV ) 一个切入山谷的系统的一个新例子位于巴西赤道的大陆人架。这条山谷从今日的海岸线扩大超过 40 km 到架裂缝,在一个被动边缘背景,在上一浅(~ 70 m ) ,狭窄(43 km ) 并且扁平(? 1 吗?? | Moab Praxedes Gomes Helenice Vital Karl Stattegger Klaus Schwarzer | 2016 | International Journal of Sediment Research2016，31，2： | 0 |
| 12 | 4万年以来巽他陆架海岸线变化的红树植物花粉记录显示文摘根据南海南部巽他陆架上的柱状剖面Sonne 18300,18302和18323的高分辨率的红树花粉记录,重建4万年以来巽他陆架的海岸线变迁历史.研究结果发现氧同位素3期时,巽他古陆上海平面较低,古陆部分出露,出露的陆架上生长了植被,有较高的花粉浓度,红树林沿巽他古陆的海岸线分布;末次冰盛期时海平面下降,巽他古陆进一步出露,海岸线的外推使红树林逐渐消失,先锋植物蕨类植物迅速覆盖在出露的陆架上;到末次冰消期,海平面上升,海岸线后退,巽他陆架逐渐又被淹没,红树林随着海岸线的迁移再次逐渐出现,并迅速拓展. | 王晓梅 孙湘君 汪品先 Karl Stattegger | 2007 | 科学通报2007，52，20： | 0 |
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