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| Registros recuperados: 15.599 | |
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| Yabe, H.; Hanzawa, S.. |
| Foraminifera are found in the Palaeozoic and Mesozoic deposits of the Netherlands East Indies. Palaeozoic forms have been described or recorded from Sumatra, Timor, Luang, and Letti, while Mesozoic ones are known not only from those islands, but also from Borneo, Java, Rotti, Halmaheira, Sula, Ceram, Great Obi, and New Guinea (?). All the Palaeozoic and Mesozoic forms, generically distinguished, are listed below, with citation of the localities and geological ages. In this list the genera except in the case of Family Fusulinidae, are arranged after J. A. Cushman's system, set forth in his „Foraminifera, their Classification and Economic Use”, 1928. Regarding this family, we rather prefer the classification of C. O. Dunbar and G. E. Condra (Bibl. 8a) to... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505689 |
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| Kruizinga, P.. |
| In arranging a list of fossil Cephalopoda of the Malayan Archipelago it soon proved that the bulk were found on Timor. On some of the other islands viz. Rotti, the Sula islands, Taliabu and Mangoli, Buru, the Misol Archipelago and Sumatra a good deal have been found also. The oldest informations on the occurrence in the Archipelago date from 1705. Rumphius described (jurassic) belemnites or dactyli idaei as he called them which were found on the island Taliabu. That old information is important as later it was the direct cause of the carrying out of further investigations on the Sula islands and in the Molucs (Verbeek, Boehm, Siboga expedition). Important material has already been found there (Brouwer, Boehm) and these discoveries are sufficient to suppose... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505878 |
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| Pannekoek, A.J.. |
| In dem Fossilverzeichnis sind die Arten in der Regel unter dem Namen aufgeführt den sie in der neuesten bei der Art zitierten Arbeit tragen ¹). Wenn eine Art in früheren Arbeiten über Niederländisch Indien anders benannt worden ist, so findet man die Nummern dieser älteren Arbeiten doch hinter dem neueren Artnamen. Der ältere, hinfällige Name ist in solchen Fallen in einer Bemerkung zu finden, ausserdem aber ist er auch in dem Artenverzeichnis aufgenommen, aber dort nur von einem Hinweis nach dem neueren Namen versehen, wo man also die zugehörige Literatur findet. Wenn von einer früher beschriebenen Art einige wenige Exemplare nach neuerer Bearbeitung zu einer anderen, schon vom selben Fundort bekannten Art gebracht worden sind, so sind diese wenigen... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505703 |
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| Wanner, J.. |
| Eine Zusammenstellung der fossilen Echinodermen des ostindischen Archipels gibt heute selbstverständlich auch nicht annähernd ein getreues Bild von dem wirklichen Umfange der Echinodermenfaunen, welche in den uns zugänglichen Ablagerungen dieser ausgedehnten Inselwelt begraben sind. Dafür ist die letztere noch viel zu wenig erforscht. Der älteste Vertreter der Echinodermen, den wir aus dem ostindischen Archipel zur Zeit kennen, ist eine von Dr. Tan beschriebene, aber noch nicht veröffentlichte und daher in der folgenden Liste noch nicht aufgeführte Poteriocriniden-Art aus dem Oberkarbon von Djambi (Sumatra). Präkarbonische Echinodermen sind möglicherweise aus Neu-Guinea zu erwarten, aber im ganzen übrigen Archipel scheint nach Allem, was wir heute über das... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505988 |
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| Beaufort, L.F. de. |
| In the following list of fishes and reptiles, known to occur as fossils in the Indoaustralian Archipelago, I have chiefly followed Smith Woodward (Bibl. 18) for the taxonomy. The teleosts, however, have been arranged according to Boulenger (The Cambridge Natural History, Vol. VII, 1904), with some slight alterations. I have not strictly followed the rules of zoological nomenclature and f. i. not changed Macrurus into Coryphaenoides. Palaeontologists are more conservative in this respect, and probably they are right. |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505950 |
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| Veldkamp, J.F.. |
| On 15 June 2002, it will be the 300th anniversary of the death of the founder of Malesian botany, zoology, and geology, Georg Everhard Rumpf, better known as Rumphius (probably late 1627-1702). It seemed suitable to present a brief commemoration here. This being a botanical bulletin, I will mainly deal with the plants. Many articles and books even have been written about this remarkable man and the results of his exploits in the Moluccas, which have given him an everlasting place of honour in the history of natural science. He is the undisputed patriarch of Malesian botany, zoology, and geology. None has had such a wide and integrated knowledge of these sciences, and was also well-versed in pharmaceutical, architectural, juridical (local and Western),... |
| Tipo: Article / Letter to the editor |
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| Ano: 2002 |
URL: http://www.repository.naturalis.nl/record/533060 |
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| Maarel, F.H. van der. |
| In connection with the particular nature of the present subject not only those publications have been used, which deal with the original type specimens or which mention the discovery from another locality, but also every publication in which new remains of the species have been described ¹). In general no use has been made of preliminary notes. An exception had to be made for those notes which hitherto have not been followed by definite descriptions. |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505589 |
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| Posthumus, O.. |
| The following enumeration contains the fossil plants, found not only in the Dutch territory, but also in the adjacent countries, the Malay Peninsula, British Borneo, Portuguese Timor and the Eastern part of New Guinea. The Philippine islands have not been considered. The classification used, is from Engler and Prantl, as given in the „Die Natürlichen Pflanzenfamilien” and the „Syllabus” of the former author. The species of flowering plants are placed in alphabetical order in the families; the species in the other classes have been arranged in larger groups. Only in some cases, still living plants were mentioned in the literature under obsolete names; in this case the fossils have been given their present names. Of the recent plants the present distribution... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505690 |
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| Krijnen, W.F.. |
| For the compilation of the map of fossil localities I have followed the example of Dr. A. Tobler (bibl. 194), arranging the localities according to age. The localities from which more than one formation has been recorded, are numbered for the oldest formation found. In the list these numbers are repeated in brackets under the heading of the other younger formations that have also been found. Thus brackets around a number are an indication that older sediments are known from the same locality. In those fossil localities are included that occur on Dutch territory and from which a collection of the fossils has been described. Vague indications in preliminary reports have not been taken into account. |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505607 |
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| Brouwer, H.A.. |
| Our knowledge of the stratigraphy of the young-paleozoic and particularly of the post-paleozoic rocks of the Netherlands East Indies is fairly extensive. Very little is known about the older paleozoic. Older paleozoic sediments are mentioned on various occasions, but the determination of the age of the rocks is mostly based on an assumption, that is made more ore less probable by the stratigraphic relation to younger fossil-bearing rocks, and not by the actual fossils, which are typical for that formation. The metamorphic rocks, which are exposed over large areas, were considered by early investigators as to belong to a very early epoch of geologic history: mostly pre-cambrian. A few fossils proved the presence of younger metamorphic rocks since. Part of... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505691 |
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| Wanner, J.. |
| Die Geologie des ostindischen Archipels hat im Laufe der letzten Jahrzehnte so beträchtliche Fortschritte aufzuweisen, dass es von Jahr zu Jahr schwieriger wird, den neuen Tatsachen und Erkenntnissen zu folgen. Auch die Stratigraphie der mesozoischen Ablagerungen dieses ausgedehnten Gebietes hat sich so rasch weiter entwickelt, dass selbst die neuesten stratigraphischen Uebersichten in den bekannten, zusammenfassenden Werken von Brouwer (21) und Rutten (86) heute in manchen Teilen schon wieder veraltet sind. Eine erneute Zusammenfassung dürfte daher nicht ohne Nutzen sein. Aus diesem Grunde bin ich gerne der Aufforderung nachgekommen, diese Aufgabe hier zu übernehmen, beschränke mich aber auf die Wiedergabe des heute vorliegenden Tatsachenmaterials, so... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505705 |
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| Bayer, Ch.. |
| In continuation of the "Catalogue of the Bursidae" (cf. „Zoologische Mededeelingen", vol. 14, p. 224, 1932), I now publish a list of the Cymatiidae in the collection of our Museum, after having revised that family. We are indebted to the work of KESTEVEN, DALL, PILSBRY & VANATTA, IREDALE, and others, for a more rational classification of the Cymatiidae. This family was formerly composed of two genera, viz. "Ranella" and "Triton" of older authors. In this century, however, as a result of researches on the dentition and the characters of the shell, these two genera have been placed into two separated families: the Cymatiidae and the Bursidae; moreover, according to the above-mentioned characteristics, the tritonoid "Ranellae", belonging to the sections... |
| Tipo: Article / Letter to the editor |
Palavras-chave: 42.73. |
| Ano: 1933 |
URL: http://www.repository.naturalis.nl/record/319113 |
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| Umbgrove, J.H.F.. |
| In his review of the palaeozoology of Java, K. Martin could in 1919, record 49 foraminifera from tertiary strata of Java, on the strength of a critical study of the existant literature, and especially on the strength of his own studies and knowledge of the above mentioned fossils (Bibl. 49). In composing the following list of the Foraminifera I have only been able to perform such a critical study for a few families. For the greater part, however, I have had to restrict myself to recording the results obtained by others, and even therein I have been obliged to restrict myself. |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505889 |
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| Rutten, L.M.R.. |
| The number of fossils that have been described from the Netherlands Territory in America is not very large. The descriptions are, however, scattered over a rather large number of publications, many of which will be found only incidentally by a reader who occupies himself intensely with the geological literature on the Antilles. It has therefore seemed to me to be a useful work to gather the data on these fossils as completely as possible, and the making of this catalogue has been especially agreeable to me, as a very large part of the fossils under discussion have been collected by Prof. Martin, in whose honour this book is edited. Some remarks may precede the catalogue. |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505964 |
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| Molengraaff, G.J.H.. |
| The oldest sediments on Curaçao are jasper¹), diabasetuff, siliceous slates²), radiolarian chert³), quartzporphyrite-crystal tuffs, porphyritecrystal tuffs, lithic porphyrite tuffs, tuffites, tuffite breccias, aphanitic crystal tuffs, tuffite-shales, graywacke-shales and graywackes4). This group of rocks — the Knip-series — is named after the plantation Knip. The stratigraphic sequence of the Knip-series is difficult to ascertain. They are intensively folded¹). I believe it would be safe to assert, that the oldest sediments of this series are jasper and diabase tuffs. The North limb of the anticlinorium in North-West Curaçao is very intensively folded, the South limb, however, in lesser degree, so that on the plantations Sint Jan, Groot St. Martha, St.... |
| Tipo: Article / Letter to the editor |
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| Ano: 1931 |
URL: http://www.repository.naturalis.nl/record/505650 |
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| Adriani, M.J.; Lensink, B.M.. |
| Kees Sipkes: florist in hart en nieren met een omvangrijke kennis van het plantenleven en met een heel eigen visie hierop. Het zijn vooral de vragen naar herkomst en verspreiding van soorten en naar de aard van het milieu, die hem steeds weer bezighouden, vooral bij het verschijnen of verdwijnen van soorten. Talrijk zijn zijn mededelingen op de ‘Floristenvergaderingen’ van de Koninklijke Nederlandse Botanische Vereniging, talrijk ook zijn tijdschriftartikelen en andere publikaties. Met vreugde begroette hij de vestiging van het Biologisch Station ‘Weevers’ Duin’ in Oostvoorne; hij speelde een belangrijke rol bij de voorbereiding van de vestigingsplaats hiervan. |
| Tipo: Article / Letter to the editor |
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| Ano: 1985 |
URL: http://www.repository.naturalis.nl/record/527004 |
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| Registros recuperados: 15.599 | |
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