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Tetrapod tracks deeply set in unsuitable substrates: Recent musk oxen in fluid earth (East Greenland) and Pleistocene caprines in aeolian sand (Mallorca) 四足动物的足迹深埋在不合适的底物中:最近的麝牛在流体土中(东格陵兰岛)和更新世的山羊在风成沙中(马略卡岛)
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2001-12-31 DOI: 10.37570/BGSD-2001-48-12
R. Bromley
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引用次数: 13
Oscar 奥斯卡
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2001-12-31 DOI: 10.37570/bgsd-2001-48-15
J. D. Friderichsen
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引用次数: 0
Festskrift i anledning af professor Asger Berthelsens 70 års fødselsdag den 30. april 1998 30日,庆祝Asger Bertelsen教授70岁生日。1998年4月
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2000-02-10 DOI: 10.37570/bgsd-1999-46-18
L. Skjernaa
This volume is in honour of Professor Asger Berthelsen on the occasion of his 70th birthday. Asger Berthelsen has made important contributions within the areas of basement geology, tectonics, structural geology, Quaternary geology, salt tectonics and deep seismic interpretations. He is an outstanding writer and illustrator.
这本书是为了纪念阿斯格·贝特森教授70岁生日而出版的。Asger Berthelsen在基底地质学、构造学、构造地质学、第四纪地质学、盐构造学和深部地震解释等领域做出了重要贡献。他是一位杰出的作家和插画家。
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引用次数: 0
Note “Paleocene” or “Palaeocene” 注:“Paleocene”或“Palaeocene”
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-12-20 DOI: 10.37570/bgsd-1999-46-17
T. Pulvertaft
There seems to be some doubt as to which of the spellings “Paleocene” or “Palaeocene” should be used in manuscripts submitted for publication in Europe, while in North America the spelling “Paleocene” is standard. The latter is not surprising, as in North America the prefix paleo- is also used in terms such as Paleozoic, paleomagnetism, etc. In Europe, however, theprefix derived from the Greek palaios (= ancient, old) is generally spelt “palaeo-”, as for example in palaeontology...................
在欧洲提交出版的手稿中应该使用“Paleocene”还是“Palaeocene”的拼写,而在北美,拼写“Paleocene”是标准的,这似乎有些疑问。后者并不奇怪,因为在北美,前缀“古-”也用于古生代、古地磁等术语中。然而,在欧洲,从希腊语palaios(=古的,旧的)衍生出来的前缀通常拼写为“palaeo-”,例如在古生物学...................中
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引用次数: 0
Crustal structure and tectonic evolution of the Tornquist Fan region as revealed by geophysical methods 地球物理方法揭示的特伦奎斯特扇地区地壳结构与构造演化
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-05-03 DOI: 10.37570/BGSD-1999-46-12
H. Thybo
Crustal structure derived primarily from geophysical investigations reveals features that may be related to the complex tectonic evolution of the Tornquist Fan region. This northwestwards widening splay of Late Carboniferous – Early Permian fault zones in the Danish region emanates from the Teisseyre-Tornquist Zone in northern Poland. Seismic reflections and velocity anomalies image collisional fault zones that formed during the Proterozoic and Palaeozoic amalgamation of the crust. Re-equilibration of Moho appears to have taken place before late Palaeozoic rifting and magmatism initiated the main phase of basin formation that continued into the Mesozoic. The resulting, strong Moho topography, with variation between depths of 26 and 48 km, has been practically “frozen in” since then, although the late Cretaceous – early Cenozoic inversion tectonics may have formed a crustal keel underneath part of the Sorgenfrei-Tornquist Zone which cuts across the Proterozoic crust of the Tornquist Fan region.
主要由地球物理调查得出的地壳结构揭示了可能与特恩奎斯特扇地区复杂构造演化有关的特征。丹麦地区的晚石炭世-早二叠世断裂带向西北扩展,起源于波兰北部的泰塞-托恩奎斯特断裂带。地震反射和速度异常反映了元古代和古生代地壳合并过程中形成的碰撞断裂带。莫霍的重新平衡似乎发生在晚古生代裂陷之前,岩浆活动开始了盆地形成的主要阶段,并持续到中生代。尽管白垩纪晚期-新生代早期的反转构造可能在索根弗雷-托恩奎斯特带的部分区域下形成了地壳龙骨,但从那时起,强烈的莫霍地形(深度在26至48公里之间)实际上已经被“冻结”了,该构造穿过了托恩奎斯特扇地区的元古代地壳。
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引用次数: 41
Wood-boring bivalves and boring linings 钻孔双壳类和钻孔衬里
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-01-30 DOI: 10.37570/bgsd-1998-45-14
S. Evans
The anatomical features and morphology and lining of the borings of wood­boring bivalves are evaluated as taxobases. The aragonitic valves and pallets have poorer preservation potential than the calcitic boring linings that some forms secrete. These linings may be septate, containing retrusive caps.
对钻木双壳类的解剖特征、孔的形态和衬里进行了分类。文石瓣和托比某些形式分泌的钙质镗孔衬里具有较差的保存潜力。这些衬里可能是分开的,包含向后的帽。
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引用次数: 24
Bioerosional evidence of rocky palaeoshores in the N eogene of Portugal: environmental and stratigraphical significance 葡萄牙晚第三纪岩石古海岸的生物侵蚀证据:环境和地层意义
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-01-30 DOI: 10.37570/bgsd-1998-45-19
C. Silva, M. Cachäo, J. Martinell, R. Domènech
Occurrences of Neogene rocky shores in Portugal have been identified by help of bioerosion trace fossils. Ichnogenera Gastrochaenolites, Entobia, Caulostrepsis, Maeandropolydora and Trypanites are generally present. The importance of bioeroded surfaces for field recognition of wave-cut platforms, hard substrate marine-flooding surfaces (transgressive surfaces), and of major interruptions (hia­tuses) in the stratigraphic record is stressed.
在生物侵蚀痕迹化石的帮助下,葡萄牙新近纪岩石海岸的出现得到了确认。一般存在鱼属胃chaenolites, Entobia, Caulostrepsis, Maeandropolydora和锥虫。强调了生物侵蚀面对于现场识别地层记录中的波浪切割平台、硬基底海洋泛水面(海侵面)和主要中断面(断裂带)的重要性。
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引用次数: 10
Commensal association of Corbula gibba (Bivalvia) and a sub-conical boring 长臂猿与次锥形钻孔的共生关系
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-01-30 DOI: 10.37570/bgsd-1998-45-15
J. Nielsen
An examination of fossil and Recent right valves of the infaunal, suspension­feeding Corbula gibba (Olivi, 1792) revealed the presence of a slender, sub- conical, unbranched boring. The boring is interpreted as the work of a commensal organism, possible a parasite. Stratigraphic range is from Eocene to Recent.
对水生悬浮物喂养的长臂猿(Olivi, 1792)的化石和最近的右瓣的检查显示,存在一个细长的、次圆锥形的、不分枝的无聊。这种无聊被解释为一种共生生物的工作,可能是一种寄生虫。地层范围始新世至新近。
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引用次数: 2
Foraminiferivory revisited: a preliminary investigation of holes in foraminifera 重访有孔虫象牙:对有孔虫孔洞的初步调查
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-01-30 DOI: 10.37570/bgsd-1998-45-16
K. Nielsen
Planktonic and benthonic foraminiferal tests from modem tropical-subtropical marine environments were investigated with regard to bioerosional traces. The traces found on the foraminiferal tests were grouped into 7 different categories. It is suggested that the different traces may be related to different unknown preda­tors of which at least one is planktonic.
研究了现代热带-亚热带海洋环境中浮游和底栖有孔虫的生物侵蚀痕迹。在有孔虫试验中发现的痕迹被分为7个不同的类别。这表明,不同的痕迹可能与不同的未知捕食者有关,其中至少有一种是浮游生物。
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引用次数: 10
Bioerosion in the carbonate budget of two Indo-Pacific reefs: La Réunion (Indian Ocean) and Mooréa (Pacific Ocean) 两个印度洋-太平洋珊瑚礁:La r<s:1>(印度洋)和moor<s:1>(太平洋)的碳酸盐收支中的生物侵蚀
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 1999-01-30 DOI: 10.37570/bgsd-1998-45-20
M. P. Clausade, N. Pari, V. Chazottes
On coral reefs, products of bioerosion through the activity of micro- and macro-boring organisms and grazers are particulate and dissolved carbonate. The con-tribution to bioerosion of the major boring and grazing species was estimated on French Polynesia and the island La Réunion. The influence of bioerosion on the calcification/dissolution budget of reefal waters and on particulate calcium car-bonate fluxes was investigated. Studies on bioerosion were performed in order to assess: (a) eroding activity of grazers through the gut content analysis of echinoids and scarid parrot fish, (b) eroding activity of micro- and macroborers from ex-perimental substrates exposed for one year, and (c) role of sponges in total bioero-sion on reefal and experimental substrates. Calcification/dissolution budget was measured using the alkalinity anomaly technique, and particulate carbonate pro-duction was analysed from trapped sediments.
在珊瑚礁上,通过微观和宏观的钻孔生物和食草动物的活动,生物侵蚀的产物是颗粒和溶解的碳酸盐。在法属波利尼西亚和拉拉西乌恩岛估计了主要的放牧和放牧物种对生物侵蚀的贡献。研究了生物侵蚀对珊瑚礁水体钙化/溶解平衡和碳酸钙颗粒通量的影响。对生物侵蚀进行研究是为了评估:(a)通过分析棘鱼和鹦鹉鱼的肠道含量来评估食草动物的侵蚀活性,(b)暴露在实验基质上一年的微孔和大孔虫的侵蚀活性,以及(c)海绵在珊瑚礁和实验基质上的总生物侵蚀中的作用。利用碱度异常技术测量了钙化/溶解平衡,并分析了捕获沉积物的颗粒碳酸盐产量。
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引用次数: 12
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