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  • 1985-1989  (253,164)
  • 1965-1969  (40)
  • 1987  (253,164)
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  • 201
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    In:  EPIC3Menschlicher Einfluß auf das Klima, Tagung Arbeitsgemeinschaft der Großforschungseinrichtungen, Bonn, pp. 25-27
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 202
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    In:  EPIC3Proc 12th Annual Conference of the International Association of Marine Sciences Libraries and Information Centers (IAMSLIC), 5-9 Oct 1987, Halifax, N S
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 203
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.437
    Publication Date: 2015-04-20
    Description: In the Bulletin of 1986 (p. 281) the revival of the PROSEA Project has been announced. Some more information on its background and progress seems in order. Historical background. In the field of plant resources of SE. Asia there are no other publications giving such thorough and comprehensive information than K. HEYNE’s ’De nuttige planten van Nederlandsch-Indie’ (1927), and I.H. BURKILL’s ’A dictionary of the economic products of the Malay Peninsula’ (1935). (For India there is the many-volumed ’Wealth of India’, which presently is being updated. Ed.). The reprint of both voluminous and outdated books in 1950 (as ’De nuttige planten van Indonesie’) and 1966, respectively, proves that there is definitely a need for such information.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 204
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.439
    Publication Date: 2015-04-20
    Description: DUNCAN, B.D. & G. ISAAC. Ferns and allied plants of Victoria, Tasmania and South Australia. Melbourne University Press, Melbourne. 1986. xii, 258 pp., line drawings, maps, b/w photogr., 8 col. pl. In Europe available from HB Sales, Littleton Road, Ashford TW15 1UQ, U.K. Ł 25.00. ISBN 0-522-84262-3. A beautifully and lavishly illustrated, thorough account of the 128 ferns and fern-allies of the Southernmost extremities of the Australian subcontinent. For the Malesian oriented scientist primarily interesting because of the excellent view it offers of a flora that is close to the Malesian flora on the generic level (almost 90% of the genera enumerated in common) and at the same time very distinct on the specific level (hardly 16% in common).
    Repository Name: National Museum of Natural History, Netherlands
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  • 205
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.413
    Publication Date: 2015-06-05
    Description: Treubia sp. New genus for Celebes. 9 May 1979. Van Balgooy 3235. Known from Asia, Pacific, America. See Pac. Pl. Areas 3 (1975) map 183. (M.M.J. van Balgooy).
    Repository Name: National Museum of Natural History, Netherlands
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  • 206
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    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi (0031-5850) vol.13 (1987) nr.3 p.391
    Publication Date: 2015-06-05
    Description: This is the first delivery of what is meant to become a long series of coloured and black-and-white photographs of ectomycorrhizae, arranged according to fungal species. Of each species a plate with four high-quality colour photographs of the mycorrhizae at different magnifications are provided together with an additional series of half-tone photographs showing important characters, such as details of structures, mantle, and rhizomorphs, both in surface views and in sections. The colour of the mycorrhizae is considered to be of prime importance for the identification of a species. A key and synoptic tables are included for determination of the mycorrhizae shown. Each year 10—15 plates will be delivered as part of a loose-leaf system. Finally this will contain 200—300 species.
    Repository Name: National Museum of Natural History, Netherlands
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  • 207
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.2 p.323
    Publication Date: 2015-03-06
    Description: Subgenus Micranthobatus is separated again from subg. Lampobatus sensu Focke (1911). The c.12 species have a scattered area of distribution, suggesting an old Gondwanan history. In Malesia five species are endemic in New Guinea (incl. New Britain), one is distributed in Borneo, the Philippines and Celebes. Two new species are described and one new variety. A key to the Malesian species is given. Remarks are made about two Australian species.
    Repository Name: National Museum of Natural History, Netherlands
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  • 208
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.2 p.313
    Publication Date: 2015-03-06
    Description: The species of Lecanopteris s.l. native to Sulawesi, Indonesia, are revised; eight species are recognized, of which L. celebica Hennipman and L. holttumii Hennipman are new.
    Repository Name: National Museum of Natural History, Netherlands
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  • 209
    Publication Date: 2014-10-27
    Description: Het doel van dit onderzoek was het verzamelen van faunistische en oekologische gegevens van Trichoptera-soorten, die voorkomen in bronnen, bronbeken, sprengen en sprengkoppen op de Veluwezoom. Hoewel we pogen met dit verslag volledigheid zoveel mogelijk na te streven, moet het niet als zodanig worden opgevat.
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
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  • 210
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.418
    Publication Date: 2015-04-20
    Description: Recently I had the good opportunity to spend three months (April to June 1986) at the Forest Research Institute in Taipei, Taiwan. In going through some of the literature, I was impressed by the number of new taxa of vascular plants discovered during the last decade or so. This is partly the result of an improvement of the transport systems and general facilities, but the main reason is the zeal and effort of several local botanists, who have made numerous expeditions to various parts of the island, particularly to the Central Range and Lanyu Islet (Botel Tobago), and also have made critical studies in the herbaria. As these new findings have been reported in various journals and books, it seemed opportune to bring the newly recorded families and genera together here.
    Repository Name: National Museum of Natural History, Netherlands
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  • 211
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.401
    Publication Date: 2015-06-05
    Description: The status of various plant systematic collections have been been discussed in S.H. SOHMER (1985) (see Bibliography), e.g. of the Philippines by D.A. MADULID, of Vanuatu by P. CABALION, a review of the herbaria of Papua New Guinea and nearby areas has been published by D.G. FRODIN (1985) (see Bibliography). The Herbarium of the University of the Philippines, at Los Baños, College, Laguna 3720, the Philippines (no formal abbreviation, ’UPLB’) encompasses in its Museum of Natural History a Botanical Herbarium (ca. 60,000 specimens), a Mycological Herbarium (CALP) (20,000), and a Forestry Herbarium (LBC) (7,500). Among the staff members are the following botanists: Ms. Norma O. AGUILAR (Curator) (general flowering plants, Leguminosae, Gramineae), E.S. FERNANDO (general trees, Palmae), W.S. GRUEZO (Compositae, Lichenes), M.R. MARTINEZ (Algae), L.S. DE PADUA (medicinal plants), J.V. PANCHO (general flowering plants, weeds), P.C. PAYAWAL (Pollen), T.H. QUIMIO (Fungi), B.C. TAN ( (Bryophyta, Pteridophyta). Affiliated staff members are I.J. DOGMA (Jr.) (Fungi) and J.P. ROJO (forest trees, Leguminosae). The institute at present specializes in the flora of Mt. Makiling, but is of course interested in the entire biology of the Philippines
    Repository Name: National Museum of Natural History, Netherlands
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  • 212
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.429
    Publication Date: 2015-04-20
    Description: Red merantis (Shorea subgen. Rubroshorea) are the most important commercial trees of the Dipterocarpaceae. In Sumatra at least 23 of the 55 species of Shorea belong to this group. Other groups are the Yellow merantis, White merantis, and the Meranti balau. We here give a key to the Red merantis based on characters of bark, twigs, and leaves. Some information on the distribution of the species in and outside the island has been added. We have found it difficult with the data available in the published record to make distributions as detailed as possible. Desch (1936, 1941) and Symington (1943) have divided Shorea Gaertn. into four groups based on timber and field characters, respectively. These groups were treated as subgenera by Meijer (1963), who gave the name Rubroshorea to the most well-known group of the Red Meranti. Anatomical studies by Gottwald and Parameswaran (1966) have confirmed the soundness of this classification.
    Repository Name: National Museum of Natural History, Netherlands
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  • 213
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    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi (0031-5850) vol.13 (1987) nr.3 p.369
    Publication Date: 2015-04-20
    Description: The ultrastructure of the ascus and the ascospores in Pseudascozonus is described. The top of the ascus opens by a small rather roughly delimited operculum. A circular furrow in the inner ascal wall causes a weakened zone. The development of the ascospore wall shows a simple homogeneous epispore and disappearance of all secondary wall material. In the epiplasm of the ascus a unique type of envelope, surrounding all eight ascospores, is described. Relationship with Ascozonus and Theleboli with 8-spored asci is suggested.
    Repository Name: National Museum of Natural History, Netherlands
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  • 214
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    In:  Gorteria : tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland (0017-2294) vol.13 (1987) nr.11/12 p.277
    Publication Date: 2015-03-11
    Description: The ecological groups (appendix 3 and 4) are defined by biotic and abiotic characteristics, in such a way that the assignment of plant species to ecological groups can be verified by means of direct measurements of the (a)biotic characteristics used. A difference with former subdivisions¹² is the fact that a species can be assigned to more than one ecological group, depending on the ecological amplitudo of the species. The (a)biotic characteristics used are vegetation structure and stage of succession, salinity, substratum, moisture regime, nutrient availability, acidity, dynamics of the ecosystem (sand drift, trampling etc.). Each characteristic has been subdivided in several classes (appendix 1). Combinations of these classes are used to define different habitat types, the so-called ecotope types. Examples of such types are: ‘grassland on dry acid soil of low nutrient availability’, or ‘woodland on wet soil of high nutrient availability’. The assignment of plant species to ecological groups has been based on ecological literature (e.g. 17, 18, 19) and has been tested by using about 20,000 relevées of Dutch vegetations. The plant species have been assigned to as many ecological groups as is necessary to explain two thirds of the occurrence of the plant species in the Netherlands, under the theoretical assumption that all habitat types are equally common. The ecological groups can be used in the analysis of ecological data, in which the occurrence of plant species is interpreted in terms of habitat factors. Computer programs have been written to determine the habitat type using floristic information as an input, assuming that the vegetation and the (a)biotical environment are in equilibrium. The ecological groups can also be used in environmental impact assessment, in studies in which changes in habitat type rather than changes in the occurrence of plant species are used to express the expected changes in the (a)biotic environment.
    Repository Name: National Museum of Natural History, Netherlands
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  • 215
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.2 p.311
    Publication Date: 2015-03-06
    Description: Lecanopteris luzonensis Hennipman is newly described from Luzon, Philippines.
    Repository Name: National Museum of Natural History, Netherlands
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  • 216
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.1 p.115
    Publication Date: 2015-03-06
    Description: New material of Knema, mainly from Borneo, necessitated the description of 5 new species, 1 new subspecies, and 2 varieties, viz. Knema latericia subsp. latericia var. subtilis, K. stylosa (stat. nov.), K. viridis, K. glauca var. riparia, K. stenophylla subsp. longipedicellata (comb. et stat. nov.), K. subhirtella, K. mogeana, and K. riangensis. Altogether 14 species are commented upon. The new taxa have been inserted in the general key and regional keys to the species as presented in Blumea 25 (1979) and 27 (1981). At present 90 species in total are recognized in Knema. An index to names of taxa supplementary to that given in 1979 has been added.
    Repository Name: National Museum of Natural History, Netherlands
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  • 217
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    In:  Leiden Botanical Series (0169-8508) vol.10 (1987) nr.1 p.3
    Publication Date: 2014-11-24
    Description: In the introduction and chapter 2 the incentives and way of reasoning are given for the description of an evolutionary basis of pollination ecology. Starting from the until recently rather anecdotical character of the study of pollination ecology as a whole, and in the absence of large-scale correlations of flowerecologically important character states with angiosperm and insect phylogeny (in the sense of Hennig, 1966), an attempt is made to derive directed evolutionary lines (transformation series) of floral character states. Because the fossil record of flowers is very restricted and the study of angiosperm phylogeny in the sense of Hennig (1966) is only at its very beginning, the only possibilities to achieve this, can be based on the comparatively well-known fossil history of insects and insect phylogeny, the least anecdotically compiled survey of insect visits to flowers, whether resulting in pollination or not, by Knuth (1898a and 1899) as far as it concerns the central European area (most thoroughly known area concerning insect fauna and angiosperm flora), and the fossil record of extant angiosperm taxa. The insect visits to flowers are correlated with the pollination-ecologically important floral character states as they are found in Hegi (1906-1931; 1963, etc.; 1966, etc.) and Knuth (1898a and 1899) by statistical analyses on an extensive data base. These analyses, based on a geographically restricted area, are correlated with the evolution of insect-feeding (and corresponding morphology) based on insect phylogeny and fossil record. These correlations require two presuppositions: “horizontal” uniformitarianism (Recent insect behaviour and physiology in taxa of lower rank are supposed to be rather constant over the world); and ”vertical” uniformitarianism (as it is used in historical geology). The results of these correlations form a series of functionally and stratigraphically/phylogenetically directed floral transformation series, dated by the fossil record of insects. The transformation series are compared with the fossil record of extant Angiospermae (for only a very minor part consisting of fossil flowers), requiring the possibility of spiral reasoning by the process of reciprocal illumination. The global scheme of the way of reasoning is illustrated in fig. 2-1. It is argued that the approach to describe evolutionary developments of pollination starting from insect fossil history and phylogeny is allowed, because in the course of evolution of insect-flower relationships, entomophilous flowers are more dependent on insect character states for (cross-)pollination, than insects are on floral character states for feeding. Free-living insects form an essential part of the environment of the “sessile” entomophilous flowers. New developments in entomophilous floral morphology are entirely dependent on the presence of corresponding insect character states. Only in case of success the, from that moment on more restricted (specialized), insect-flower relationships give rise to genuine co-evolution of anthophilous insects and entomophilous flowers. In chapter 3 the material and statistical methods are described, in addition to some prospects of this study in building a more refined survey, up to an analysis on the basis of extensive pollen analyses on the loads of the integuments and contents of the digestive tracts of central European Cetoniinae, Lepturinae and Cerambycinae of which the results are presented in the appendix. In chapter 4 a survey is given of the feeding-habits of the adult insects included in the present study as mentioned in Knuth (1898a and 1899) and of their relatives, giving a systematically complete survey of the feeding-habits of Coleoptera, Hymenoptera, Lepidoptera and Diptera (with some remarks on anthophilous insects of other orders), with stress on the taxa in which anthophily developed. The main conclusion of this survey can be that of many families the feeding-habits were not found in the more general entomological literature, and also in more specialized literature the feeding-habits in many cases are imperfectly known. Chapter 5 deals with the correlation of the anthophilous feeding-habits of insects with their phylogeny and fossil record. The correlations are restricted to the insect orders in which the main anthophilous insects occur: Coleoptera, Hymenoptera, Lepidoptera and Diptera. Comparison of the monophyletic Holometabola with their sister-group the Paraneoptera indicates that the original feeding-habits of both larvae and adult insects of the former were saprophagous and/or fungivorous in moist vegetable debris and similar substances (as already suggested by Tillyard, 1926). In describing the possible sister-group relationships within the Holometabola a non-pollination ecological conclusion is made: it is concluded that, if feeding on the blood of warm-blooded animals can be considered a synapomorphy in the Siphonaptera (fleas), they could not have originated earlier than in the Triassic (up to now, presumed origin of the Mammalia and Aves, see Romer, 1966); this is in contrast to Hennig (1981) who placed the origin of this order in the late Permian. In discussing the correlations of the feeding-habits of the taxa of lower rank with their fossil record and phylogeny within the orders mentioned above, the following conclusions are drawn. Coleoptera The habitat of the earliest Coleoptera most probably was that under the (loose) bark of trees. This habitat formed the selective pressure which favoured the adaptive development of elytra from the forewings. The earliest Coleoptera (Ommadidae) may have fed on reproductive structures or flowers as early as the lower Permian. In the upper Triassic this type of feeding must have been established, because all polyphagan series were present in that time (may be only some are of lower Jurassic origin). During the Jurassic the Polyphaga in which anthophily developed radiated considerably and in the upper Jurassic they were fairly well-differentiated (see tables 5-1 and 7-1). During the Cretaceous the differentiation of these beetles had a much slower rate, but, regarding the rather extensive differentiation in the upper Eocene to lower/middle Oligocene, at the end of the Cretaceous the origin may have laid of many (stem-groups) of families. The following reconstruction of relationships between anthophilous Coleoptera and reproductive structures and/or flowers can be made. After a fairly rapid radiation during the upper Triassic and Jurassic, in the Cretaceous only few developments took place, but correlated with the ecological break-through of the Angiospermae in the Upper Cretaceous, the differentiation rate increased again. Because it is not known when the origin of the Angiospermae has to be placed in the geological time scale (see below), in table 7-1 the stratigraphical appearance of extant insect taxa in which anthophily developed is given from the upper Triassic to the Lower Cretaceous. Hymenoptera The original feeding-habits of the Hymenoptera most probably were fungivorous. The habitat originally may have been decaying vegetable debris, but the Symphyta s.str. most probably lived in crevices of bark and under (loose) bark. The latter habitat probably formed the selective pressure which favoured the adaptive development of the cenchri, providing the possibility of fixing the wings in crawling under bark. The evolutionary developments towards and within hymenopteran anthophily were correlated with those in the maternal care and social behaviour. The earliest Hymenoptera (Xyelidae) may have fed on reproductive structures and/or flowers as early as the Triassic. The extant families of the Symphyta s.str. in which anthophily developed, differentiated from about the lower/middle Jurassic onwards and were definitely established in the upper Jurassic (see tables 5-2 and 7-1). In the Lower Cretaceous the earliest Apocrita appeared (Ichneumonoidea) and in the Upper Cretaceous an extensive differentiation of wasp families, in which, mainly nectarivorous, anthophily developed, can be observed (table 5-2). The differentiation of the Apoidea was about completed in the upper Eocene to lower/middle Oligocene and this may mean that the earliest Apoidea or their direct predecessors were already present in the uppermost Cretaceous. The following reconstruction of relationships between Hymenoptera and reproductive structures and/or flowers can be made. After a fairly rapid differentiation in the Jurassic of the Symphyta s.str., only some differentiations in the Apocrita, in which anthophily developed, took place in the Lower Cretaceous, followed by an increased differentiation after the ecological breakthrough of the Angiospermae and of the nectarivorous (aculeatan) wasps in the Upper Cretaceous. Probably in the same time the Apoidea originated and differentiated very rapidly during the (uppermost Cretaceous and) early Tertiary. The stem-group of the Bombinae and Euglossinae must have been present in the upper Eocene to lower/middle Oligocene. In correlating the feeding-habits with the phylogeny and fossil record of the Aculeata s.str. a pollination-ecologically interesting character state was met in the Bradynobaenidae. Although no feeding-habits were found for this family, the pinnate setae of its subfamily Typhoctinae may indicate close relationships with flowers (parallel evolution of setae as in Apidae). The morphology of the Bradynobaenidae urgently requires further research into their feeding-habits and behaviour. Lepidoptera When the Lepidoptera definitely originated within the Amphiesmenoptera (Lepidoptera + Trichoptera) is not known, but the earliest, mandibulate, certain Lepidoptera were present in the lower Cretaceous (Micropterigidae) and probably their predecessors were already present in the upper Jurassic. The Micropterigidae most probably fed on pollen in those times. The Ditrysia were very differentiated in the middle Tertiary. This differentiation (see table 5-3), particularly that of the Papilionoidea, indicates a much earlier origin. It is suggested that after the mandibulate, pollen-feeding phase, the development of a longer haustellum induced a rapid differentiation of the higher Lepidoptera after the ecological break-through of the Angiospermae in the Upper Cretaceous, and mainly took place in the uppermost Cretaceous and early Tertiary. Diptera The earliest probably pollen-feeding Diptera are found in the Bibionomorpha which were present in the upper Triassic (whether Tipulomorpha, Psychodomorpha and Culicomorpha also had relationships with reproductive structures and/or flowers in that time, or only developed nectarivorous anthophily from the Upper Cretaceous onwards, is not known). A rather rapid differentiation of Diptera, in which anthophily developed, can be traced in the Jurassic (see tables 5-4 and 7-1). During the Cretaceous new differentiations in dipteran anthophily hardly took place, but the extensive established differentiation of Brachycera in the upper Eocene to lower/middle Oligocene indicates a much earlier origin. It can be suggested that after the ecological break-through of the Angiospermae the anthophilous, mainly nectarivorous Brachycera differentiated rapidly in the uppermost Cretaceous and first half of the Tertiary. Chapter 5 is concluded with a survey of the stratigraphical appearance of the insect taxa in which anthophily developed. In chapter 6 the statistical analyses of the central European flower visits of insects and their association with floral character states are carried out. The differentiated survey of the correlation of the feeding-habits with the phylogeny and fossil record is narrowed to insect taxa of higher rank: Coleoptera, Diptera, Lepidoptera and Hymenoptera (section 6.1). The last order is divided into two groups, viz. the Apoidea and non-apoid Hymenoptera on the basis of their different morphology and (in many cases) behaviour (Apoidea being nearly obligatory anthophilous). Generalized special morphological character states are indicated for the insect groups (lengths of mouth parts). The interdependence of insects and floral character states is correlated with the results of chapter 5 (correlation of feeding-habits with the phylogeny and fossil record of the insect taxa in which anthophily developed). With regard to the complex of facultative and obligatory pollination types (section 6.2), it is concluded that the more specialized insect-flower relationships developed during the latest Cretaceous and became finally established in the middle Tertiary (possibly with the exclusion of more specialized pollination by beetles, which may have evolved earlier). The earliest Angiospermae, then, most probably were non-specialized entomogamous, depending at their time of origin, on pollination by Coleoptera, Diptera and non-apoid Hymenoptera (Symphyta). Comparison of the frequencies of obligatory pollination types within the complex of facultative and obligatory ones, indicates that bees and butterflies reached the highest degree of specialization of insect-flower relationships as far as it concerns the central European area (section 6.2.2). With regard to the obligatory pollination (section 6.2.2), corresponding with the pollination syndromes, it can be stated that obligatory myiophilous flowers (not sapromyiophilous) with some depth effect may have existed from about the middle Cretaceous onwards and gave rise to melittophilous and psychophilous flowers in the (uppermost Cretaceous and) early Tertiary, while at the same time the obligatory form disappeared. Phalaenophilous flowers developed later in the Tertiary. In the blossom-pollinator relationships (section 6.3) the following can be suggested. Allophilic flowers occurred in the earliest Angiospermae. Hemiphilic flowers may have originated in the late Cretaceous, giving rise to euphilic flowers in the early Tertiary. As regards the development of flower types (section 6.4) it can be stated that actino- or already pleomorphic flowers occurred in the early Cretaceous. From about the middle Cretaceous somewhat stereomorphic flowers, particularly with regard to pollination by longer-rostrate flies, developed, and may have given rise to zygomorphic flowers. Stronger zygomorphic and stereomorphic flowers became functional during the early and middle Tertiary. Among the earliest Angiospermae the following blossom classes (section 6.5) may have been present: inconspicuous entomophilous blossoms, dish- to bowlshaped blossoms and possibly some type of brush-shaped blossoms (the last ones not specialized for longer-tongued insects). From about the middle Cretaceous developments towards bell- and funnel-shaped blossoms were possible. In the late Cretaceous possibly more trumpet- and tube-shaped blossoms may have become functional and developed during the early Tertiary. Gullet-shaped blossoms are of later Tertiary origin. Flag-shaped blossoms are known from the late Paleocene. As regards the single flower as a pollination unit versus (small-flowered) inflorescences (section 6.6) it is argued that the most plesiomorphous entomogamous Angiospermae had single flowers as pollination units (considering only the size of the flowers with regard to the size of their potential pollinators; the flowers were arranged in inflorescences, see section 7.1) and the development of small-flowered inflorescences took place under the selective pressure of ovule damage by larger, mandibulate, partly anthophagous pollinators, through plants or large inflorescences with small flowers, dependent on pollination by minute insects. The more compact inflorescences are adapted to pollination by larger and stronger-flying pollinators with the advantage of some spreading of the small one- or few-ovuled ovaries. The development of small-flowered plants and inflorescences could have taken place very early in the evolution of the angiosperm flowers. The developed or rudimentary perianth (section 6.7) cannot be correlated to certain insect groups. Absence of perianth parts is mainly characteristic for anemophilous flowers. With regard to floral colours (sections 6.8.1 and 2) a comparison is also made between the taxa of lower rank by reciprocal averaging. In the comparisons the colour vision of insects is also included. One of the results of the analyses is, that in all insect groups the most plesiomorphous, anthophilous representatives mainly visit yellow (and white) flowers. The most plesiomorphous angiosperm floral colour most probably indeed was yellow (this may be supported by floral biochemistry). The total result consists of the following transformation series: —from (green) yellow to white: very early in angiosperm evolution; —from white to blue and blue-mixed colours: starting in the late Cretaceous; —from yellow or white to red and red-mixed colours: starting in the late Cretaceous; —from blue or blue-mixed to red and red-mixed colours and vice versa: from the late Cretaceous onwards. It generally can be stated that floral colours in the course of angiosperm evolution fanned out from the middle of the spectrum towards the extremes; towards the short wave-lengths in connection with pollination by higher Apoidea and Lepidoptera; towards the longer wave-lengths in connection with pollination by certain taxa of Lepidoptera and, later, birds. Cryptantherous flowers (section 6.9) may have been present from the late Cretaceous onwards, perhaps sapro-entomophilous inflorescences excluded. In the numbers of stamens per flower (section 6.10) the following developments could have taken place. The earliest Angiospermae most probably had many stamens. In conjunction with the developments towards smallflowered plants and inflorescences, reduction of the numbers may have occured very early in the evolution of the angiosperm flowers. Considering that obligatory anemophilous flowers have only very few stamens per flower, this can be regarded as an apomorphous condition. In larger flowers in the second half of the Cretaceous the stamens could become reduced in numbers, in connection with specialization of the pollination. With regard to the position of the ovaries (section 6.11), it can be stated that the selective pressure (mandibulate, anthophagous insect visitors, mainly beetles) favouring the development of half- to entirely inferior ovaries existed from the very origin of the Angiospermae and was probably completed very early. In the number of ovules per stigmatic surface (mostly corresponding with the carpel) (section 6.12), the number of ovules increases with an increase of the specialization of the pollination. The earliest entomogamous Angiospermae probably had few ovules per carpel. Reduction to one took place in the development to small-flowered inflorescences and anemogamy. Increase in specialized pollination types probably started in the Upper Cretaceous and early Tertiary in connection with specialized longer-tongued pollinators. As regards nectar presence and position (section 6.13) it appeared that it cannot be suggested on the basis of the statistical analysis whether the earliest Angiospermae had pollen or nectar-containing flowers. It is demonstrated that beetles in many cases (also) feed on pollen on nectar-containing flowers (see also the tables in the appendix). In the position of the nectar the following transformation series exists: from free by way of half-concealed to entirely concealed nectar. In the variation in time between receptivity and dehiscence (section 6.14.1) it is demonstrated that anemophilous flowers most often are protogynous, although this is also common among entomophilous flowers. Facultative and obligatory homogamy is mostly found in the obligatory pollination types. Protandry appears to be almost exclusively restricted to entomophilous flowers, but it requires adjacent developments to guide visiting insects over the flower or inflorescence by colours and/or odour and nectar, to optimalize the chance of cross-pollination. It is argued that a gymnospermous sister group of the Angiospermae most probably was protandrous, because of the fact that, in case of endosperm proliferation before fertilization, the simultaneous presence of pollen and endosperm in hermaphroditic, entomophilous reproductive structures has to be minimalized to avoid insect injury to the endosperm. In the case of homogamy and protogyny too much endosperm would be present simultaneously with the pollen, and mandibulate insect visitors (beetles and possibly also symphytan wasps) would easily feed both on pollen and proteinrich endosperm. In order to avoid endosperm injury, the simultaneous presence of endosperm and pollen must have included a minimum quantity of the first and have lasted as short as possible. This circumstance can only occur in protandrous conditions. Moreover protandry representing the most logical sequence of ripening of the end of a stem, the simultaneous presence of pollen and endosperm, given the insects present in those times, must have prohibited the development of absolute homogamy and protogyny (avoiding too much “advertized” endosperm in entomophilous, hermaphroditic conditions). Because protandry, however, requires adjacent “guiding”-developments, which obviously did not take place in the Gymnospermae, a selective pressure on the hermaphroditic reproductive structures, favouring cross-pollination, favoured the development of unisexual flowers (with a good chance to become anemogamous), and another selective pressure led to the development of “double fertilization” in which the endosperm only starts proliferation after fertilization. Once established, the “double fertilization” opened the way for the development of homogamy and protogyny. The formation of stigmatic surfaces can be considered an adaptation to avoid fertilization-decreasing pollen droplet-feeding by, also non-mandibulate, insects (flies). Analysis of the protandry in several families of the central European area, particularly in the Apiaceae, indicated that this type of dichogamy easily leads to the development of unisexual flowers, as so to avoid too much selfpollination. Protandrous flowers more often are self-incompatible than are protogynous ones. Protandry appears to be more characteristic for unspecialized entomophilous pollination types, than for specialized ones (creating second order herkogamy in the former; in the more specialized flowers, particularly in melittophilous ones herkogamy is present morphologically). The presupposition of this section was that unspecialized, mandibulate, injurious insect visitors may have formed the selective pressure favouring the development of second order herkogamy. The analysis does not support this. Dichogamy is developed under the selective pressure of optimalizing crosspollination, in protandry easily leading to unisexual flowers. Absolute homogamy (section 6.14.2) more often occurs in specialized insectflower relationships than in unspecialized ones. In the latter case it may induce the development of unisexual flowers (but to a lesser degree than does protandry). In more specialized pollination types it may have induced development of heterostyly, and under unfavourable pollination conditions it easily led to cleistogamy. In the developments towards dicliny (section 6.15) the following difference between anemogamous and entomogamous species is hypothesized. The difference of directability of the pollen vectors led to an enlarged chance of development of monoecy under protandrous/homogamous, anemogamous conditions and of dioecy under similar entomogamous conditions. The abundance of hermaphroditic protogynous flowers in anemogamy requires extension of the definition of the syndrome of anemophily: “unisexual flowers, in case of monoecy protogynous, or protogynous hermaphroditic flowers”, in stead of solely “unisexual flowers”. In section 6.16 the preceding evolutionary developments are outlined in a series of functionally and stratigraphically/phylogenetically directed transformation series. Chapter 7 deals with the reconstruction of the evolutionary developments in pollination ecology. In hypothesizing the theoretical model of the earliest angiosperm flowers (section 7.1) by considering the plesiomorphous states of many of the transformation series, added with some comparative-morphologically derived ones, the following conclusions were drawn. The earliest angiosperms most probably had the following character states. The pollen flowers were arranged in inflorescences, most probably leafy cymes, and were of intermediate size. They were hermaphroditic, protandrous and allophilic, non-specialized entomophilous, pollinated by beetles, symphytan wasps and oligoneuran (possibly mainly bibionomorphan) and possibly asiliform flies. Their general appearance was dish- to bowl-shaped, paleomorphic. The optical attractant was formed by the stamens and discoloured upper leaves (to some degree already perianth-like); the floral colours most probably were yellow and white. The many stamens were arranged in bundles which represented compound sporangiophores, bundles being formed in a phyllotactic spiral, continuing that of the floral envelopes. The stamen filaments were short. The gynoecium consisted of probably many superior, petiole-like stiped, at anthesis not entirely closed, carpels, which were infolded cupules with sessile stigmas. Each carpel contained a few ovules in a laminar or submarginal position. Double fertilization was present. The basic synapomorphy of the Angiospermae is the double fertilization and it strongly indicates an entomophilous, hermaphroditic origin. The indication of a selective pressure favouring the development of double fertilization, may favour the possibility of a polyphyletic origin of the Angiospermae. But the restricted possibilities of hermaphroditism in their predecessors and the probable uniqueness of this development, may indicate monophyly. In the food supply for insect visitors it is hypothesized that in first instance the fertile parts (being the most attractive for insect visitors) provided food in the following transformation series: 1) from plain stigma to stigma with glandular warts; 2) from stamens to staminodes; 3) from plain stamens to stamens with glandular bodies at the base of the filament; 4) from plain stamens to stamens with glandular bodies at the apex of the connective; 5) from plain staminodes to staminodes with glandular bodies; 6) from stamens with glandular bodies to staminodes with the same; The staminodes with glandular bodies occasionally may have given rise to tepals and petals with nectaries. In increasing the attraction of the flowers, laminar stamens were derived from stamens with a slender filament and by reduction of the upper leaves. The laminar stamens gave rise to tepals by way of laminar staminodes. This means that there more probably is question of sterilization of laminar stamens, than of the reverse. In the remarks on the origin of the Angiospermae (section 7.2) it is concluded that there may be possibilities of temporary presence of hermaphroditic reproductive structures in the Bennettitales (demonstrated) and Gnetales (most probably). In the Pentoxylales these are not known. The development of double fertilization is functionally explainable, and thereby it is less probably a development according to the “economy principle”. The probable entomogamy of the earliest Angiospermae may include that the “upland” theory is superfluous, because entomophilous pollen is quantitatively rare in stratigraphical pollen analysis. In section 7.3 the apomorphies of the transformation series mentioned in section 6.16 are approximately dated on the basis of the fossil record and phylogeny of the insect taxa in which anthophily developed. Added is the dating of ornithophilous and chiropterophilous pollination types, based on the fossil record of birds and bats in which anthophily developed, respectively. In section 7.4 the fossil record of extant angiosperm taxa is correlated with the dated apomorphies in section 7.3. For each taxon an estimation is made of the pollination type, based on the presence of extant insect taxa in which anthophily developed in the period in which the angiosperm taxon appeared, and on the basis of the type of fossils (macrofossils or fossil pollen) and the abundance of the fossil pollen. The types of angiosperm fossils may form an indication of the pollination type of the flowers they represent. There are three possibilities: 1) if in a period macrofossils are present and fossil pollen of the same taxon is not found in stratigraphical pollen analysis, or does not occur in some abundance (pollen not originating from the macrofossils), there is a major chance that the fossils represent entomophilous (or otherwise zoophilous) flowers; 2) if in a period both macrofossils and in considerable quantities fossil pollen of the same taxon are found (pollen not originating from the macrofossils), there is a major chance that the fossils represent anemophilous flowers; 3) if only stratigraphical pollen is found in considerable quantities, it most probably represents anemophilous flowers. Analysing the survey of fossils of extant angiosperm taxa at the end of this section, it is concluded that fossil pollen representing entomophilous flowers in quantitative, stratigraphical pollen analysis is rare and occurs irregularly in time (qualitatively, however, more entomophilous than anemophilous pollen types are found). Macrofossils qualitatively more often represent entomophilous than anemophilous flowers. Pollen morphology also can give an indication of the pollination type: sculptured, tectate (and sticky) pollen mostly is entomophilous and psilate, and atectate (dry) pollen mostly is anemophilous. With regard to the pollination type, it is suggested that entomophilous pollen is longer on its way from locule to stigma, than is anemophilous pollen, and therefore more urgently needs a protective layer of “pollenkitt” to avoid desiccation; at the same time it functions as adhering agent to the body of the pollen vector. It is suggested that the columellate sculpture of the exine keeps the protective “pollenkitt” equally distributed over the pollen surface, and that the combination of sculpture and “pollenkitt” has a function in itself in the relation of adhering to the body of the pollen vector and the deposition on the stigmatic surface. Because recent investigations indicate the presence of columellate pollen in as early as the Triassic and because also in gymnosperms evidence for relicts of columellae is found, and the earliest angiosperms most probably were entomogamous, it is suggested that the earliest angiosperm flowers had columellate pollen, which would mean that atectate, psilate pollen (as e.g. in the Degeneriaceae) has to be regarded as apomorphous. The correlation of the extant angiosperm taxa with the above mentioned elements indicates the following appearance of floral character states in the stratigraphical periods: Barremian-Albian —anemophilous flowers, including possibly already inconspicuous, green flowers with reduced perianth, few stamens and a reduced number of ovules per stigma (carpel); the presence of this apomorphous pollination type and its corresponding probable character states indicate a much earlier origin of the Angiospermae; —some more obligatory beetle pollination; —possible sapro-entomogamy; —somewhat hemiphilic flowers are possible (in connection with more obligatory beetle pollination); —possible haplomorphic flowers; —actino- and pleomorphic flowers; —probable (partial) sympetaly; —dish- to bowl-shaped blossoms; —brush-shaped blossoms (not specialized for longer-tongued insects); —small-flowered inflorescences; —yellow and white floral colours; —reduction of the numbers of stamens per flower in connection with smallflowered entomophilous inflorescences; —reduction of numbers of ovules per stigma (carpel) in connection with smallflowered inflorescences; —possible protogyny; —possible unisexual flowers. Cenomanian-Turonian —early more obligatory myiogamy; —more obligatory cantharogamy; —early more obligatory wasp pollination; —earliest somewhat stereomorphic and possibly zygomorphic flowers (e.g. margin flowers of small-flowered inflorescences); —earliest possible bell- to funnel-shaped blossoms; —larger solitary flowers; —possibly some blue and blue-mixed colours in connection with early more obligatory myiogamy; —peri- and epigyny; —nectar-containing flowers with open nectar. Coniacian-Santonian-Campanian —possible very early pollination by Apoidea or their
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  • 218
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.527
    Publication Date: 2015-06-05
    Description: The specimens collected by J.R. and G. FORSTER on Capt. COOK’s second voyage around the world are widely dispersed in at least 15 European herbaria. Apparently no single institution has a full set, and no attempt has been made to account for and lectotypify the names of taxa based on this material. Since numbered collections with duplicates in the modern sense were not made, there are usually no proven isotypes of either holotypes or lectotypes. I am attempting to list published lectotypifications of Pacific Island taxa based on Forster material and to assemble information needed to choose suitable lectotypes where these have not been chosen and published previously. I will appreciate information on published lectotypifications and on the location and identity of Forster specimens not already annotated by me. F.R. Fosberg, U.S. National herbarium, Smithsonian Institution, Washington – D.C. 20560, U.S.A.
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  • 219
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.446
    Publication Date: 2015-04-20
    Description: Editorial note: Traditionally we have included literature references on nonvascular plants. We have, however, the impression that few, if any, are interested in this information, as we hardly ever get any reaction from scientists engaged in these fields. Cryptogamists, moreover, often give no inkling as to the distribution of their taxa, which makes the scanning of their literature a timeconsuming and unrewarding business. Therefore, unless serious protests are received, and unless specialists offer their assistance in compiling the relevant literature, we intend to save ourselves space and a lot of time, and propose to delete the sub-chapters a) and b) starting with the next volume.
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  • 220
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.380
    Publication Date: 2015-06-05
    Description: Tree Flora of Indonesia checklists under editorship of Dr. T.C. WHITMORE and Dr. I.G.M. TANTRA (Forest Dept., Bali). Sumatra has now been distributed at least to at least a few key Institutes outside Indonesia. Others can write to either Ir. Rubardi, or Ir. K. Sumarno, Forest Research & Development Centre, Bogor, for a copy while the limited stocks last. Sulawesi proofs were corrected in November 1986.
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  • 221
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    In:  Flora Malesiana Bulletin (0071-5778) vol.40 (1987) nr.9/4 p.421
    Publication Date: 2015-04-20
    Description: Among the papers left by the late Dr. Van Steenis the following manuscript was found, nearly finished. It seemed of sufficient interest to botanists on holiday who can’t leave the local flora alone. Just because one’s mind is elsewhere during holidays beaches are undercollected areas and interesting finds may be expected. It must be understood that this is a key to the common species in natural formations on sandy or rocky substrates, e.g. of the sandy beach, the beach forest, the pes-caprae- and Barringtonia-formations, but not of the seagrass- and mangrove-formations. There are many species that have only a limited distribution, or occur only sporadically, or, especially in tourist-infested areas, are actually inland weeds. These have not been included as a key to them all was beyond the idea of this note. At the end a list of some rarely, or facultatively natural occurring species is given by family. Any species seen that has not been enumerated here is not necessarily an addition on a rare one, yet, one never knows, of course, and it would be prudent to collect some of it for a second look back home, where it may serve at least as a souvenir of a good time.
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  • 222
    Publication Date: 2015-04-20
    Description: Thirteen new species and a new variety of Psathyrella are described: P. badia, P. bernhardii, P. borgensis, P. capitatocystis, P. dennyensis, P. minutissima, P. mookensis, P. multicystidiata, P. perpusilla, P. ploddensis, P. romseyensis, P. twickelensis, P. vyrnwyensis, and P. obtusata var. aberrans. Some rectifications in the keys published in our monograph (Kits van Waveren, 1985) and some reconstructed keys necessitated by the insertion of new species are given. Recently described new species from outside the area covered by our monograph are briefly described and discussed. Corrections in and supplementary information to some of our descriptions in the monograph and a redescription of P. obtusata are presented.
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  • 223
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.1 p.157
    Publication Date: 2015-03-06
    Description: In Malesia and Australia there are nine species of Oryza L. (Gramineae). Oryza meyeriana (Zoll. & Mor.) Baillon has two varieties. Oryza schlechteri Pilg. is only known from Irian Jaya (Indonesian New Guinea). Oryza australiensis Dom. and O. meridionalis Ng are endemic to Australia. The numerous forms of O. sativa L. have not been treated. Oryza rufipogon Griff., supposedly the wild progenitor of O. sativa, is considered as a distinct species. The name for the subfamily Oryzoideae is validated.
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  • 224
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.2 p.303
    Publication Date: 2015-03-06
    Description: Male reproductive axes are described which have three pairs of decussate bracts, some with free axillary groups of stamens. The developmental stages are demonstrated by scanning electron microscopy (SEM). The view, earlier advanced for the female counterparts, that these reproductive axes are reduced polyaxial systems, is supported.
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  • 225
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    In:  Blumea - Biodiversity, Evolution and Biogeography of Plants (0006-5196) vol.32 (1987) nr.1 p.91
    Publication Date: 2015-03-06
    Description: Lerchea Linn., a genus from Sumatra and Java, is revised. Eight species are recognized. Two new species, L. corymbosa and L. parviflora, are described. One variety has been raised to species, L. beccariana. A key, descriptions, illustrations, and distribution maps for all species are provided. Raphides are shown to be present in Lerchea and the two closely related genera Xanthophytum and Pomazota. Hence these three genera are transferred from Pomazotoideae-Pomazoteae to Rubioideae-Hedyotideae. Two cladograms are given, one of Lerchea, the other showing the relationship between Lerchea, Xanthophytum, and Pomazota.
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  • 226
    Publication Date: 2014-10-27
    Description: The mid North Atlantic between 24°N and 55°N along 30°W and between 20°W and 30°W along approx. 25°N, investigated by the AMNAPE cruises in the four seasons, spring (1980), summer (1983) autumn (1981) and winter (1982), is dominated by Temperate waters with a northern and southern branch of the North Atlantic Drift, Subtropical Sargasso Sea waters in the south and Subarctic waters in the north (Yen der Spoel, 1981, 1986; Van der Spoel & Meerding 1983; Pafort- van Iersel, 1985). The present study gives the relation of the microplankton distribution in the upper 5m of the water column with the hydrography and seasons.
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  • 227
    Publication Date: 2014-10-27
    Description: Three new species of Cynopotamus Valenciennes, 1849 are described, C. gouldingi n. sp., C. juruenae n. sp. and C. tocantinensis n. sp. New diagnoses and synonymies are provided for most species of this genus as a consequence of the results from a study of recently collected specimens. A revised key to all valid species is presented.
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  • 228
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 229
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    In:  EPIC3Annals of Glaciology, 11, pp. 180-183
    Publication Date: 2019-07-17
    Description: In 1980-81, 1983-84, and 1985-86 airborne surveys with the electromagnetic reflection (EMR) system were made of Ekström Ice Shelf, Antarctica. The EMR data were supplemented by measurements of surface elevation with radar altimetry during flights at a constant pressure altitude. The accuracy measurements of ice thickness in areas with clearly developed bottom reflectors was used to generate a plot of surface elevation against ice thickness. The effect of changing barometric pressure during flights could be reduced by this means. Elevations were calibrated over the open sea at the beginning and end of each flight. On the basis of these data, the surface elevation, ice thickness and isostatic anomalies have been mapped over the ice shelf.
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  • 230
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    In:  EPIC3Nature, 327(6120), pp. 318-319, ISSN: 0028-0836
    Publication Date: 2019-07-17
    Description: The Ronne Ice Shelf, floating between Berkner Island and the Antarctic peninsula, is the biggest ice shelf in Antarctica. It drains an estimated 1.2 × 106 km2 of the Antarctic ice sheet, much of it resting on bedrock below sea level. Consequently, the balance and dynamics of this ice shelf is of importance to Antarctic glaciology, especially with regard to the integration of this part of the cryo-sphere into the global processes that control the climate of the Earth. Extensive radio-echo sounding (RES) by Robin and others revealed reflections in the central part of the Ronne Ice Shelf at the relatively shallow depth of 100–200 m below surface1. The interpretation of these echoes, which varied in strength, was ambiguous, and the possibility of internal reflecting horizons was thoroughly discussed. But after surface elevation measurements by radar altimeter from drifting balloons appeared to fit the presence of thin ice, it was decided to base a thickness map of the Ronne Ice Shelf on these RES echoes1–4. We now present direct observational evidence from boreholes that the total ice thickness is much greater than mapped, and that the shallow RES reflections therefore do come from internal horizons.
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  • 231
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    In:  EPIC3Berichte aus dem Institut für Meereskunde, Kiel, 173, 132 p.
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
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  • 232
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    USGS
    In:  EPIC3Washington, USGS
    Publication Date: 2016-02-01
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 233
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    SPRINGER
    In:  EPIC3Boundary-Layer Meteorology, SPRINGER, Bounda(41), pp. 241-249, ISSN: 0006-8314
    Publication Date: 2016-07-18
    Description: After introductory remarks on similarity laws to be satisfied in wind tunnel experiments simulating small-scale meteorological processes, mean and turbulence characteristics of wind tunnel boundary layers are presented and compared with the characteristics of the atmospheric boundary layer. The results are used to evaluate the possibilities and limitations of physical modeling of pollutant dispersion in general. In the second part of the paper, the potential of wind tunnels to solve micro-meteorological problems of real practical interest will be demonstrated. The example involves the investigation of the effects of building downwash on ground-level concentrations for flue gases discharged from natural draft wet cooling towers.
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  • 234
    Publication Date: 2016-02-15
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 235
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 236
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 237
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    In:  EPIC3Proceedings of the International conference on "Heavy Metals in the Environment", New Orleans, 1987, pp. 239-241
    Publication Date: 2019-07-17
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    Publication Date: 2019-07-17
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  • 239
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    Alfred Wegener Institute for Polar and Marine Research
    In:  EPIC3Alfred-Wegener-Institute for Polar- and Marine Research, Bremerhaven, Bremerhaven, Alfred Wegener Institute for Polar and Marine Research
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  • 240
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    Zeitschrift für Gletscherkunde und Glazialgeologie
    In:  EPIC3Innsbruck, Zeitschrift für Gletscherkunde und Glazialgeologie
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
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    Zeitschrift für Gletscherkunde und Glazialgeologie
    In:  EPIC3Innsbruck, Zeitschrift für Gletscherkunde und Glazialgeologie
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    Repository Name: EPIC Alfred Wegener Institut
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  • 242
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    Archiv für Lagerstättenforschung der geologischen Bundesanstalt
    In:  EPIC3Wien, Archiv für Lagerstättenforschung der geologischen Bundesanstalt
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
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  • 243
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    Institut für Meteorologie und Geophysik der Universität Innsbruck
    In:  EPIC3Innsbruck, Institut für Meteorologie und Geophysik der Universität Innsbruck
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  • 244
    Publication Date: 2014-08-14
    Repository Name: EPIC Alfred Wegener Institut
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  • 245
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    IfM Hamburg
    In:  EPIC3Hamburg, IfM Hamburg
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  • 246
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    NSF
    In:  EPIC3Washington, D.C., NSF
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  • 247
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    Archiv für Lagerstättenforschung
    In:  EPIC3Wien, Archiv für Lagerstättenforschung
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  • 248
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
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  • 249
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    NGU
    In:  EPIC3Norway, NGU
    Publication Date: 2016-07-29
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    Zeitschrift für Gletscherkunde und Glazialgeologie
    In:  EPIC3Innsbruck, Zeitschrift für Gletscherkunde und Glazialgeologie
    Publication Date: 2015-03-26
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  • 251
    Publication Date: 2022-05-04
    Description: The brackish water plathelminth fauna of New Brunswick, Canada is compared to European brackish water biotopes. 48 species are identified, 7 new species are described, and 7 species are presented though the material was insufficient for a species description. From 48 brackish water species, 37 (77 %) are amphi-atlantic. Hypotheses for an explanation of such a high similarity are discussed.
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  • 252
    Publication Date: 2022-05-04
    Description: At the island of Sylt, North Sea, the plathelminth fauna of supratidal salt marshes was investigated. A total of 103 species is recorded, 75 of which were found throughout the year. These species are truely brackish. 78% of them perform univoltine life-cycles. Salinity, oxygen, and water availability are less stable in salt marshes than further seaward in the tidal zone. Many plathelminth species are able to encyst when conditions deteriorate. Thus they can withstand intermittend harshness. It is shown that every common plathelminth species prefers a distinct range of salinity. In species capable of encystment, every change in salinity causes a change in abundance. Regarding all plathelminth species, salinity affects the species composition. The plathelminth distribution pattern is determined by (1) salinity, (2) oxygen availability, and (3) temperature. Together with differences in ground relief, water content, sediment composition, vegetation density, and insolation these factors form a patchy environment. Sites of similar combination of factors are patchily distributed, and plythelminth distribution matches these mosaics. Thus, the distribution of species non-random in salt marshes. A modified index of 'mean crowding' (Lloyd 1967) is proposed to describe the distribution of species in patchy environments. From the distribution pattern, the combination of the factors preferred is extracted. Closely related species differ in the preferred ranges, and their niches overlap to a small extent only.
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  • 253
    Publication Date: 2022-05-04
    Description: Environmental conditions in salt marsh creeks are intermediate between the open tidal coast and estuaries. A large salt marsh creek at the island of Sylt (North Sea) was studied in order to test whether its fauna is more similar to that of the open tidal coast or to that of estuaries. Because of a sandy bar at the seaward opening, the tidal range is only 10 cm in the creek, and the water level never drops below the level of the sand bar. Zoobenthos in the sandy bottom and on the sandy shores was studied at both ends and in the middle of the creek. Polychaeta and Plathelminthes were determined to species level. On an average, 2115 metazoans were found below 10 cm2 of surface area. At the seaward end of the creek, abundance and taxonomic composition are similar to that of the adjoining Wadden area. Nematoda are the dominant taxon, followed by Copepoda, Plathelminthes and Oligochaeta. Taxonomic composition is different at the landward end. Plathelminthes and Nematoda are most abundant followed by Copepoda. Both Oligochaeta and Polychaeta are scarce at these newly eroded sites. Plathelminth abundance at the landward end of the creek is exceptionally high (770–935·10 cm−2). Contrary to what is generally found in estuaries, the species density of Plathelminthes shows a significant increase toward the land. The species composition of Polychaeta and Plathelminthes indicates that the sites below mean high tide level of the creek correspond to the adjacent eulittoral Wadden area while the fauna of the supralittoral sites of the creek is similar to the fauna of supralittoral tidal coasts. Typical sublittoral species did not occur in the salt marsh creek. Thus, salt marsh creeks may be regarded as a small-scale model for the tidal coast. In context with the results obtained, the definition of estuaries is discussed.
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  • 254
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    In:  EPIC3Helgoländer Meeresuntersuchungen, 41(1), pp. 83-111, ISSN: 0174-3597
    Publication Date: 2022-05-04
    Description: During recent years, many investigations on small zoobenthos have been performed at the island of Sylt. As these studies were carried out sporadically over many years and as different extraction methods were used, comparisons of the results have been hampered. Therefore, in August/September 1986, 24 sites were sampled and evaluated using one quantitative method throughout. Sites range from mud to exposed sand and from the sublittoral to the supralittoral. Macrofauna and the taxa Plathelminthes, Polychaeta, and Oligochaeta are determined to species level. Macrofaunal (〉0.5 mm) abundance is highest in mud and continuously decreases with increasing exposure to wave action. Meiofaunal (〈0.5 mm) abundance is less variable. Nematoda dominate in mud and muddy sand, Copepoda in sheltered and exposed sand, other taxa only intermittently. Related to surface area, no correlation between macro-and meiofaunal abundance is apparent. Plathelminthes and Copepoda reach highest abundance per surface area in sand but their per volume density is higher in mud and muddy sand. Related to sediment volume instead of surface area, the meiofaunal abundance pattern is very similar to the macrofaunal pattern. The faunal composition changes gradually along the tidal gradient without general faunal boundaries. On an averange, the faunal similarity of neighbouring sites is highest in Oligochaeta and lowest in Plathelminthes. Presumably, Oligochaeta tolerate wider ranges of environmental factors. This may explain the low number of oligochaete species. On the other hand, Plathelminthes seem to adapt to relatively narrow ranges of factors and their species richness is highest. Because of macrofaunameiofauna interaction it is suggested that the meiofaunal assemblage will be least stable in mud and muddy sand, and most stable in exposed sand.
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  • 255
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    In:  EPIC3Microfauna Marina, 3, pp. 249-260
    Publication Date: 2022-05-04
    Description: 5 new species of free-Iiving Plathelminthes are described from supralittoral salt marshes and the intertidal-supralittoral transition belt of the island of Sylt (North Sea). Macrostomum bicurvistyla, M. brevituba, Placorhynchus tetraculeatus, and Zonorhynchus pipettiferus belong to well known genera. The genus Moevenbergia (Promesostomidae, Brinkmanniellinae) with the type-species M. una differs from all known genera of Brinkmanniellinae in having paired receptacula seminis and lacking a bursa copulatrix destinctly separated from the atrium genitale.
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  • 256
    Publication Date: 2019-07-16
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  • 257
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    In:  EPIC3Journal of experimental biology, 131, pp. 89-105
    Publication Date: 2019-07-16
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  • 258
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    In:  EPIC3Kolloquium, Institut für Meereskunde, Kiel.
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  • 259
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    In:  EPIC3Mitteilungen aus dem Institut fuer Geophysik und Meteorologie der Universitaet zu Koeln,Heft 54.
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  • 260
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    In:  EPIC3Quantum Aspects of Molecular Motions in Solids, A. Heidemann, A. Magerl, M. Prager, D. Richter and T. Springer (Eds.), Berlin, Springer-Verlag, pp. 93-97
    Publication Date: 2019-07-17
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  • 261
    Publication Date: 2019-07-17
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  • 262
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    In:  EPIC3Vibrational Spectra and Structure, 16, pp. 142-225
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  • 263
    Publication Date: 2019-07-17
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  • 264
    Publication Date: 2019-07-17
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  • 265
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    In:  EPIC347. Jahrestagung der Deutschen Geophysikalischen Gesellschaft, 31 März - 4 April, Clausthal-Zellerfeld.
    Publication Date: 2019-07-17
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  • 266
    Publication Date: 2019-07-17
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  • 267
    Publication Date: 2019-07-17
    Description: To elucidate how the brain processes information, the functioning of neuronal networks has to be analysed. We developed a multi-neuron recording system that is able (1) to record several neurons with one multi-unit microelectrode, (2) to separate the multi-unit data into single-unit spike trains and (3) to display the neuronal activity, especially the interactions between the different single units, in real-time. The system consists of two PDP-11/73 laboratory computers, each extended with a TMS-32010 based TZQ-11 coprocessor. One computer is programmed to detect and classify spikes from the electrode signal. The second computer does further data processing and controls the experimental procedure (Generation of stimuli etc.).
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  • 268
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    In:  EPIC3Journal of geophysical researchA9), 92, pp. 9949-9961
    Publication Date: 2019-07-17
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  • 269
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    In:  EPIC3Reports on Polar Research, 39(87), pp. 140-141, ISSN: 0176-5027
    Publication Date: 2019-07-17
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  • 270
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    In:  EPIC3Reports on Polar Research, 39(87), pp. 222-227, ISSN: 0176-5027
    Publication Date: 2019-07-17
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  • 271
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    In:  EPIC3Microchimica acta,III, pp. 123-140
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  • 272
    Publication Date: 2019-07-17
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  • 273
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    In:  EPIC3ICES Council Meeting,H/45
    Publication Date: 2019-07-17
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  • 274
    Publication Date: 2019-07-17
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  • 275
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    In:  EPIC3Reports on Polar Research, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, 35, 126 p.
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  • 276
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    In:  EPIC3Botanica Marina, 30, pp. 233-241
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  • 277
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    In:  EPIC3S Afr J mar Sci, 5, pp. 467-470
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  • 278
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    In:  EPIC3ICES Council Meeting,H/46
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  • 279
    Publication Date: 2019-07-17
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  • 280
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    In:  EPIC3Menschlicher Einfluß auf das Klima Tagung Arbeitsgemeinschaft der Großforschungseinrichtungen, Bonn, 1987, pp. 21-24
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  • 281
    Publication Date: 2019-07-17
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  • 282
    Publication Date: 2019-07-17
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  • 283
    Publication Date: 2019-07-17
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  • 284
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    In:  EPIC3Chemosphere, 16(10), pp. 2487-2496
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  • 285
    Publication Date: 2019-07-17
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  • 286
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    In:  EPIC3Remote Sensing from Space: Proc of the International Colloqium, University of Oldenburg, FRG, pp. 187-202
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  • 287
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    In:  EPIC3ICES Council Meeting
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  • 288
    Publication Date: 2019-07-17
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  • 289
    Publication Date: 2019-07-17
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  • 290
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    In:  EPIC3Aquat Mamm, 13, pp. 119-121
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  • 291
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    In:  EPIC3European Cetacean Society meeting, pp. 33-38
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  • 292
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    In:  EPIC3
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  • 293
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    In:  EPIC3Inst Ant Chil Ser Cient
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  • 294
    Publication Date: 2019-07-17
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  • 295
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    In:  EPIC3ICES Council Meeting,H/47
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  • 296
    Publication Date: 2019-07-17
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  • 297
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    In:  EPIC3Marine Micropaleontology, 11, pp. 311-332
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  • 298
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
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  • 299
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    Physikalisch-Technische Bundesanstalt
    In:  EPIC3Braunschweig, Physikalisch-Technische Bundesanstalt
    Publication Date: 2015-03-16
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  • 300
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    Zeitschrift für Gletscherkunde und Glazialgeologie
    In:  EPIC3Innsbruck, Zeitschrift für Gletscherkunde und Glazialgeologie
    Publication Date: 2015-04-16
    Repository Name: EPIC Alfred Wegener Institut
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