ALBERT

Description: Twelve species of terricolous microlichens from the Angmagssalik District, Southeast Greenland, are reported: Caloplaca friesii, C. livida, Lecanora boligera, Lecidea oligotropha and Leciophysma arctophila, which are new to the lichen flora of Greenland, Rinodina conradi, which is new to the eastcoast, and Baeomyces roseus, B. rufus, Buellia geophila, B. punctata, Caloplaca tornoensis and Mycoblastus tornoensis, new to Southeast Greenland. In a discussion of the greenlandic distribution, unpublished records from the herbarium of Copenhagen (C) are incorporated. Notes on the habitats are given and the pertinent phytosociological units indicated. Some morphological and anatomical characters are commented upon briefly.

Description: The three species Galium silvaticum L., Galium aristatum L. and Galium schultesii Vest show differences in morphology, cytology and geographical distribution. These differences are described and discussed. Crossing experiments between the three species were without results. No hybrid could be obtained. Galium silvaticum, Galium aristatum and Galium schultesii must be considered as separate species.

Description: The 16 recognized species of Sorocea are listed with their synonyms and distribution. Two new taxa are described: S. steinbachii C.C. Berg and S. hirtella Mildbread ssp. oligotricha Akkermans & Berg. Three new combinations are made: S. muriculata Miquel ssp. uaupensis (Baillon) C.C. Berg, S. trophoides W. Burger ssp. rhodorachis (Cuatrecasas) C.C. Berg, and S. sprucei (Baillon) Macbride ssp. saxicola (Hassler) C.C. Berg. A key to the species is presented.

Description: The species Polypodium banaense C.Chr. is transferred to Crypsinus. The recognition of a genus Phymatopteris Pic. Ser. (= Phymatopsis J.Sm.) separate from Crypsinus is discussed.

Description: The six species of Curtia, including a hitherto undescribed species published here, as well as the monotypic genus Hockinia can be distinguished from each other by the seed coat structure. The anticlinal walls and the cuticle provide the most useful information. Curtia tenuifolia appears to be a complex species, but subsp. tenella can be readily separated from this complex by the seed coat structure. Heterostyly has been found in C. tenuifolia subsp. tenuifolia, C. obtusifolia, and Hockinia montana, but differences in seed coat structure can not be correlated with long-, short-, and equal-styled flowers. The differences in seed coat structure, the length of the seeds, and the number of cells per seed plead for maintaining Hockinia (closely related to Curtia) as a distinct genus. One new species of Curtia is described and a new combination is made.

Description: SETTEN, A. K. van & KOEK-NOORMAN, J.: Studies in Annonaceae. VI. A leafanatomical survey of genera of Annonaceae in the Neotropics. — Bot. Jahrb. Syst. 108: 17—50. 1986. — ISSN 0006-8152. Within the scope of the multidisciplinary research project on systematics of Annonaceae, a survey of the leafanatomical features and their distribution in the neotropical Annonaceae is presented. The studied specimens form a rather homogeneous group, as may appear from the family description given here. A detailed study of the leafanatomical features reveals, that differences are mainly found in the indument, the position and contents of the idioblasts, the structure of the primary vein, the type of crystals in the epidermal cells, and the type of sclereids. Based on character states, phenetic similarities and differences are discussed and compared with the classifications of FRIES (1959) and WALKER (1971).

Description: One new species of Dorstenia from Brazil is described: D. carautae C.C. Berg, and four new combinations are made: D. cayapia Vellozo subsp. asaroides (Hooker) C.C. Berg, D. cayapia Vellozo subsp. paraguariensis (Hassler) C.C. Berg, D. cayapia Vellozo subsp. vitifolia (Gardner) C.C. Berg, and D. ramosa (Desvaux) Carauta, Valente & Sucre subsp. dolichocaula (Pilger) C.C. Berg. A list of and a key to the 22 Dorstenia species distinguished in south-eastern tropical America are presented, together with synonymy and distributional data.

Description: Recently a multidisciplinary investigation program on the systematics of Annonaceae was started at Utrecht with special emphasis on the Neotropics. This project will be carried out largely within the framework of the UNESCO-project Flora Neotronica. The first goal is to provide a modern classification of the family as a whole, the second is the publication of a series of monographs for Flora Neotropica. The project has been planned and started in close consultation with leading botanists on the Neotropical flora. The Annonaceae are a family of pantropical distribution with between 2000 and 2500 species in ca. 130 genera as presently understood. In the Neotropics the family is represented by ca. 750 species and 35 genera. It is a family of trees, shrubs, and lianas. Its place is within the order of the Magnoliales and its supposedly closest relative is the family of the Myristicaceae. The Annonaceae, although generally considered primitive in many features, nevertheless offer a number of specialized features as well This makes it a promising object using various kinds of comparative morphological, karyological, and anatomical data. Besides, many species are of medicinal or commercial value, such as various species of Annona and Rollinia, the fruits of which are commonly eaten in most countries of Central America and South America; the Soursop (Annona muricata) is widely cultivated throughout the tropics.

Description: Vochysia sectio Ciliantha Stafleu, subsectio Ferrugineae Warming. A V. vismiifolia Spruce ex Warming stipulis incrassatis, foliis lanceolatis longe acuminatis, floribus calcari longo modice incurvo, petalo intermedio stamen aequante, stigmate terminali parvo instructis differt. Holotypus: “coll. unknown” (comm. D. Allen) in U, fl. 14 Nov. 1953. PERU, Nanay River near Iquitos, altitude 100 m., “quillo sisa”, tree more than 100 feet high, on clayey soil about 20 feet above river (Isotypes: US 2104976, Y 47782).

Description: A new species of Asterophorum, A. mennegae, is described from the Sipaliwini Savanne (Suriname). The position of Asterophorum within the family is briefly reviewed, and a key to the 2 species is given.

Description: The wood and leaf anatomy of representatives of the 9 genera of the Opiliaceae are described in detail. It is possible to separate the genera on the base of both wood- and leaf anatomical characters. Herein the presence of cystoliths of varying shape and size is important. Some comments on the taxonomy and possible phylogeny of the familiy are given.

Description: In his introductory statements to 'The Symposium on the Phylogeny and Classification of the Filicopsida' which was held in London, 1972, HOLTTUM, when dealing with 'dubious groups of relationships which would particularly repay investigation', mentioned the Polypodiaceae first (HOLTTUM, 1973: 6). Talking about Polypodiaceae the present authors deal with the Polypodiaceae sensu stricto only, thus excluding the Cheiropleuriaceae, Dipteridaceae, Grammitidaceae, and also the Loxogrammaceae, taxa which were formerly (or are still) included in the Polypodiaceae sensu lato. As delineated in this way, this almost exclusively pantropical family consists of about 600 species and an indefinite number of genera.

Description: The new species Coussapoa manuënsis C.C. Berg is described.

Description: Lolium perenne L. staat in de flora’s opgegeven als zodevormend. In het algemeen is dit stellig juist. Wat echter aan floristen minder bekend zal zijn, naar aan grasland-specialisten eerder, is dat er rassen van L. perenne bestaan die korte, ondergrondse uitlopers vormen. Schrijver dezes was er tenminste nogal verwonderd over van Engels Raaigras, groeiende op de kade van het Noorderhoofd in het westelijk havengedeelte van Amsterdam de “grasbosjes” aan korte uitlopers ontsproten te zien. De vindplaats net resten van veekoeken maakte het waarschijnlijk, dat hier agrarische producten verladen werden en dat de L. perenne-planten van aangevoerd “graszaad” afkomstig zijn. Landtouwliteratuur verschafte spoedig de gewenste inlichtingen. In “Ons Grasland” door W.P. Cnossen (Uitgave P. Noordhoff, 1947) staan op p. 32 uitstekende foto’s van uitlopersvormend Engels Raaigras. Genoemd geschrift bevat op p. 7 een overzicht van verschillende grassen, die boven- en ondergrondse uitlopers kunnen vormen, waarin deze soort ook is opgenonen. Asmus Petersen, “Die Graser” (Akademie-Verlag, Berlin, 1953) geeft op p. 140 de uitspraak van de graslandexpert C.A. Weber, dat het uitlopersvormende Engels Raaigras voor weidegrasland hij uitstek geschikt is en de teelt ervan aanbeveling verdient. Hoewel niet floristisch, is het misschien aardig er gewag van te maken, dat Cnossen nog wel een bezwaar vermeldt tegen het uitlopersvormende Eng. Raaigras nl., dat de in de nazomer aan uitlopers ontstane spruiten slecht bewortelen en door het vee gemakkelijk worden losgetrokken (plukken); overal over het land liggen dan de grasrestjes verspreid. Er zijn zeker nog wel meer vermeldingen aangaande deze uitlopersvormende rassen van Engels Raaigras te vindon. Voorstaande opgaaf is maar een greep.

Description: Van Polygonum cuspidatum zijn mij de volgende vier standplaatsen op de Veluwezoom tiekend: 1. Bronbos van de Hemelse Berg te om bronnen en langs bronbeekjes, Alno-Ulmion-vegetatie, bodem jong, nitraat- en humusrijk slibhoudend zand, iets zuur, beschaduwd. 2. Oever van het beekje door het Zwijersdal te Oosterbeek, noordelijk van de oude kerk; Polygonum ouspidatum-facies, licht bodem jong, humusrijk zand, zuur. 3. Verdroogde beekbodem, zuidelijk van de weg Arnhem-Dieren, bij Daalhuizen, Velp; fragmentaire Alno-Ulmion-vegetatie met Polygonum cuspidatum-facies, licht bodem jong, humusrijk zand, zuur. 4. Oever van de Beekhuizerbeek ter hoogte van de grote vijver. Beekhuizen hij Velp; Alno-Ulmion-vegetatie, bodem jong, humusrijk zand, zuur. Voor alle vier standplaatsen geldt het volgende: Polygonum cuspidatum wordt tot 2½ meter hoog en bedekt grote, gesloten oppervlakten, waardoor de bestaande vegetaties zeer verarmd worden; alleen Ranunculus ficaria handhaaft zich goed en kan plaatselijk, zoals b.v. op de Hemelse Berg, de gehele bodem bedekken.

Description: In ons land is Galanthus nivalis L. „vrij algemeen, doch steeds verwilderd” (Bekn. Schoolflora, 8e druk). Het blijft daarbij in het midden gelaten van hoe lang geleden zulk een verwildering stamt. In sommige gevallen (De Kaagoevers; de omgeving van Leimuidon) is de situatie ter plaatse van die aard, dat men aan een zeer grijs verleden gaat denken. Het begrip verwildering zou dan nog slechts inhouden, dat de plant oorspronkelijk verwilderd is en in deze zin ware het ook van toepassing op sommige andere soorten, die men als regel niet verwilderd noemt. Werkelijke datering is bij ons weten echter nergens mogelijk en daarmee blijft het probleem onopgelost. Wij willen daarom iets meedelen over een vindplaats ten opzichte waarvan althans een vaag vermoeden van datering kan worden uitgesproken. In het dorp Warmond kan men naar het Westen afslaan langs de Kloosterlaan. Even vóór de plaats waar deze zich in een pad door de weilanden verliest, ligt aan de Zuidzijde van de weg een nagenoeg cirkelvormige akker, omringd door een ongewoon diepe sloot waaromheen een ringvormige met struikgewas bezette strook, die wederom door oen sloot omgeven is. Vlak hierbij stond in do late middeleeuwen het mannenklooster Marienhove. De vorm van do akker wekt overigens meer associaties met een burcht, dan met oen klooster on inderdaad werd het klooster (volgens de .gangbare beschrijvingen der Warmondse kastelen en kloosters) in 1413 gesticht „op een woeste of verlaate plaats, Oud-Tellingen genaamd.” Door sommigen wordt dit geïnterpreteerd als een aanwijzing, dat, nog vroeger, het kasteel of tenminste de „hofstede” Oud-Teilingen hier stond; anderen projecteren de ligging daarvan enige honderden meters zuidelijker.

Description: Op 14 Jan. 1952 vond de heer E.E. van der Voo op een oud bruggetje ten noorden van Woerden, gemeente Kamerik, oen groeiplaats van Asplenium trichomanes. Hiervan werd melding gemaakt in een rapport van do Afd. Natuurbescherming van het Staatsbosbeheer van de hand van de heer J. van der Veer (14 April 1955). Dit rapport kwam ter kennis van Ir. N. Roorda van Eysinga, Directeur van het Zuid-Hollandsch Landschap en deze verzocht de heer Kipp, Bosbouwkundig Ambtenaar van de Prov. Planologische Dienst on mij de groeiplaats te bezoeken en plannen voor te bereiden het gehele bruggetje zo nodig naar elders over te brengen, wanneer dit gevaar liep door de eigenaar afgebroken te zullen worden. Dit gevaar is niet denkbeeldig want de muren staan niet goed recht meer en alle dergelijke bruggetjes in de omgeving zijn in de loop der jaren reeds door meer solide bouwsels vervangen. Bij het bruggetje aangekomen zag ik op 18 Dec. 1956 direkt een 100 tal prachtige planten van de genoemde Asplenium trichomanes tegen het oostmuurtje.

Description: 1. Occurrence.--Lemnaceae may occur in stagnant or sluggish streaming waters, specially in ditches, pools, streamlets, inundated rice-fields, etc. They are also found in all other waters in which larger swamp plants offer anchorage to the tiny Lemnaceae. They can be expected between stands of sedges, grasses, cat’s-tail, etc. or between or under swimming water plants, for example Azolla, Eichhornia, waterlilies, etc. The smallest Lemnaceae, consisting merely of a rootless globule, Wolffia, which is always submerged, is easily escaping attention under other water plants. 2. Collecting.--Lemnaceae are mostly found in sufficient quantity and can easily be collected in a bottle or plastic bag. In case they are sparse and small (Wolffia) the use of a wire—netting (old coffee sieve) may be handy. They are kept wet in the bottle or plastic. If they should be kept for several days or longer they should be stored in an open container with a small amount of earth added; the container should be kept in the shade.

Description: IUCN, says the paper Categories, Objectives and Criteria for Protected Areas, ”is dedicated to the wise use of the Earth’s natural resources and to the maintenance of the Planet’s natural diversity.” What to think of the sequence? Use first, maintain second? And this comes from the International Union for the Conservation of Nature and Natural Resources? ”The World National Parks Congress, taking place in Bali, Indonesia, October 11-22, 1982, will provide case studies from around the world to illustrate how the various categories of protected areas are meeting the needs of countries of all economic, social, cultural, and political backgrounds,” writes J.A. McNeely, the secretary of the Commission on National Parks and Protected Areas, in a special issue of the Swedish journal Ambio (11: 237. 1982). ”No longer just playgrounds for vacationers and means for conserving natural heritage, protected areas have become an inseparable part of the modern human ecosystem.”

Description: Mrs. Delia D. Adefuin, Museum Research Assistant, Manila, is pursuing her M.S. in Botany degree. She is currently the Secretary of the Fern Society of the Philippines. She is working on the Fern Flora of Metro Manila and is preparing the manuscript of a pictorial encyclopedia which will include descriptions of species and horticultural recommendations. Miss Barbro Axelius (S) collected and studied Xanthophytum and Lerchea (Rubiaceae) in Sarawak, Kalimantan and Sumatra, August 1982- February 1983.

Description: Tropical Botany in Aberdeen University. This was started by Professor J.W.H. Trail, who held the chair from 1877 to 1919, and travelled in the Amazon Valley (1873-75) mainly collecting cryptogams and studying palms. He was succeeded by Prof. W.G. Craib (1920-33) who was never in the tropics but devoted his work to the Flora of Siam, based on the collections of A.F.G. Kerr, and assisted by Miss E.C. Barnett. After a considerable lag, tropical botany was revived by the energetic efforts of Dr. P. Ashton as lecturer in systematics and ecology of the eastern tropics, establishing ties with Malayan colleges in teaching and research. This is at present perpetuated by two lecturers, Dr. K. Jong and Dr. M.D. Swaine, the latter’s experience lying largely in the tropics of West Africa. In addition Dr. N.M. Pritchard, Dr. J.B. Kenworthy and Dr. G. Hadley have been on secondment to the University of Malaya, while Dr. I. Alexander made research visits to India, Ghana and Peru. Over the years the Department has provided undergraduate and research training to innumerable students from many different tropical countries, some of which attained responsible posts, e.g. Prof. E. Soepadmo. Important courses in tropical biology are given, not available elsewhere in the U.K. (started 1973). The benefits for Aberdeen students is important: amongst others they led to expeditions to various parts of the tropics, recently to Sabah and to the Ivory Coast. Royal Society Tropical Rain Forest Collaborative Research Programme. Arising out of a feasibility study by Dr. T.C. Whitmore and P.F. Cockburn, the theme ’Recovery of tropical rain forest after disturbance’ was adopted as the initial basis of the programme. Possible territories for the research include Sabah and the Philippines. Detailed plans for a 5-year project are being prepared in consultation with colleagues in Southeast Asia.

Description: Bentham, G. & J.D. Hooker, Genera plantarum. Cf. W.T. Stearn on its history and dates of publication in J. Soc. Bibl. Nat. Hist. 3 (1956) 127-132.

Description: 9th Pacific Science Congress, Bangkok. According to the Preliminary Announcement the Congress will take place Nov. 18- —Dec. 9, 1957. Organising chairman is M.C. Lak Kashemsanta, Dep. of Agriculture, Bangkok. Fifteen general subjects have been entered for contributing papers and discussion, viz: (a) Problems confronting tropical botanical institutions, (b) Vegetation types of the Pacific basin, (1) Tropical, (2) Temperate, (c) Ethnobotany of Thailand and contiguous countries, (d) Vernacular names of Pacific plants. (e) Phycology in the Pacific basin. (f) Algal ecology, with special reference to coral reefs and atolls. (g) Bibliographic problems in the natural sciences in the Pacific. (h) The teaching of botany and the training of botanists in the tropics. (i) Systematics, evolution and distribution of Pacific plants, (j) Botany of medical plants in the Pacific basin, (k) Forest botany in the Pacific basin. (l) Botany of agricultural plants and weeds. (m) Plant ecology in the Pacific. (n) Mycology and phytopathology in the Pacific. (o) Plant physiology in the Pacific. Besides, a special symposium on Climate, Vegetation, and Land Utilization in the Humid Tropics, sponsored by Unesco, will be convened by Dr F.R. Fosberg.

Description: It is with the utmost regret that we announce the sudden and quite unexpected death of Dr. Marius Jacobs, editor of this Bulletin. See the obituary on page 3869. He was co-editor of the Flora Malesiana Bulletin for nr. 17 (1962) to nr. 22 (1968) and took full responsibility onwards of nr. 27 (1974). He showed great ability in enlarging its scope and we have many letters in our archives expressing appreciation and admiration for the lively and informative style in which he edited the Bulletin. I had to take over the editorial work for this number at short notice, but I was greatly helped by a number of Rijksherbarium colleagues, which help is gratefully acknowledged. In this way the delay has been kept to a minimum. It is, however, possible that some news items etc. have not been printed and that information submitted to Dr. Jacobs has not been entered due to this sudden change of editorship. I offer my apologies if this has happened and hope that (if still relevant) the news will again be forwarded to the new editor, Dr. J.F. Veldkamp, Rijksherbarium, who will take over starting next number.

Description: On p. 475 it was erroneously mentioned that Miss S. Darnton accompanied Miss W.M.A. Brooke in Sarawak; she rightly collected in North Borneo.

Description: The next monographic study which will be undertaken for the series Pteridophyta of the Flora Malesiana will be devoted to the tree ferns of the Cyatheaceae. In connection with the large size of these plants and the desirability of having more and complete material at our disposal, the following notes are addressed to field collectors who may be in a position to obtain specimens. For securing essential parts tree ferns appear less unmanageable than they may look at first sight.

Description: Abeywickrema, B.A.: The genera of Ceylon Pteridophytes (Ceyl. J. Sc. A. Bot. 13, 1956, 1-30). Keys & descr. – & M.D. Dassanayake: Crenidomonas bilabiatum (Nees & Bl.) Copel., a fern new to Ceylon from Ritigala (Ceyl. J. Sc. A. Bot. 13, 1956, 41-42, t. 2).

Description: The Botanical Survey of India continued to make collections during 1982, with the following results: Andaman & Nicobar Is.: Shola Bag, Mt Harriet, Jirkathang, Poona Nallah, Saddle peak, Diglipur, Rutland I. & Little I., 2875 specimens. Arunachal Pradesh: Various areas of Kameng Distr., Subansiri Distr., 9750 specimens. Assam: Garampani, 60 specimens. West Bengal: Darjeeling, Jalpaiguri, Hollong, Jaldapara, Chilapata, Salkumar, Daidaighat, Barasat, 2665 specimens. Bihar: Madhuban, Nimiaghat, Paresnath Hills, 315 specimens. Dehra Dun: Chakrata, Missoori, 325 specimens. Gujrat: Catchment and submergence areas of Sipu Reservoir Project, 1505 specimens. Kerala: Trichur, Idduki, Silent Valley, Valra Reserve Forest, Cannanore, Trivandrum, 3770 specimens. Madhya Pradesh: Kanha National Park, Chhodarpur Distr., 1190 specimens. Maharashtra: Areas of Jalgaon Distr. and Buldhana Distr., 4390 specimens. Manipur: Cherrapunjee, Mawphlong, Sorharim, areas of West Khasi Hills Districts, 2000 specimens. Rajasthan: Bharatpur, Desert National Park, 1605 specimens. Sikkim: Rangpo, Singtham, Bumbing, Manuring, Duga, Pandam, Takchi, Meli, areas of Gangtok, Chungtham, Lachi, Thanga, Panthang, 2590 specimens. Uttar Pradesh: Gori & Kali Valley, Chittoragarh Distr., 500 specimens.

Description: Dr P. Vermeulen, Amsterdam, who had obtained the 1955 grant of the Netherlands Buitenzorg Fund went via India, where he spent a month above Darjeeling, to Bogor; he also paid a visit to Queensland, his chief interest being the study of Orchidaceae. In returning he made a trip in Central Sumatra with Dr Meijer; he arrived in Holland end Dec. 1956. Mr L.L. Forman, Kew, who was granted a year leave for work at the herbarium Bogoriense, Bogor, made various trips in Indonesia, collecting in W. Java, Bali, North-east Celebes, and joining Dr Kostermans on a forest survey in East Borneo.

Description: The ultrastructure of the spore walls of Beenakia dacostae (Beenakiaceae, Gomphales) has been studied. Spore walls are mainly composed of a distinct episporium and a thick, dark, ornamented ectosporium. The general structure is identical with that of other members of the Gomphales, such as Gomphus and Ramaria

Description: Merrill (Philip. J. Sc. 2, 1907, Bot. 284) based Mearnsia on specimens collected from Mount Halcon in the Phillipines and dedicated the genus to Major Mearns who accompanied him on the expedition. Merrill described the flowers of the sole species (M. halconensis) as 4-merous with 8 stamens and 2 carpels and the capsule as dehiscing by ‘a single slit at the apex only and inside the persistent calyx tube’.

Description: In Malesia the genus Tephrosia is represented by 20 species, native or introduced and naturalized, including 6 subspecies and 5 varieties; 4 species are restricted to Malesia. Two of these species are newly described: T. barbatala and T. elliptica; the former includes one new variety (var. glabra). Two new subspecies and one new variety are distinguished: T. filipes subsp. longifolia, T. purpurea subsp. barbigera, and T. maculata var. elongata. Two taxa are given a new status: T. maculata var. appressepilosa and T. pumila subsp. aldabrensis. Four species, T. dichotoma, T. repentina, T. coarctata, and Kiesera sumatrana are for the first time sunk into synonymy. A key to the taxa, synonymy, and full descriptions with plates and distribution maps are given.

Description: During identification and study of the materials of the genus Blepharis Juss. in the Central National Herbarium (CAL) of the Botanical Survey of India the authors came across some specimens (Lawson 314) from Tavancore, which was identified as B. molluginifolia aff But critical study revealed that the typical molluginifolia is a different species from which the new taxon can be distinguished by several characters. The species is named after M.A. Lawson who collected the specimen for the first time.

Description: One new species of Aristolochia, A. singalangensis, from Sumatra is described here. This is the only Malesian species to have the fruit dehiscing from the apex towards the base. Remarks are given for some Asiatic and Malesian species, all belonging to Aristolochia except one to Thottea, on their taxonomy, nomenclature, typification, characteristics for identification, relationship, distribution, etc. The phenomena and significance of aristolochiaceous plants-butterflies relationship have been discussed. Germinated pollen grains have been found in dehisced anthers of open flowers in both Aristolochia and Thottea. Pollination of the Aristolochiaceae has been concisely reviewed.

Description: After the completion of my revision of Lepisanthes (Blumea 17, 1969, p. 33—91) I paid a visit to the herbaria at London (BM) and Kew (K). This led to a few alterations and additions, the main of which are the following.

Description: As explained in Takhtajan’s preface this book is not a mere translation of his ‘The origin of Angiospermous plants’ (1961, in Russian), but an entirely new book. I find this true and not true. Comparing it with the Origin (1958 translation of the 1954 Russian version) the essence of the new book was there given in a nutshell. In size, chapter subjects, argumentation, and bibliographic documentation, the work is very much extended and it makes very interesting reading indeed. The sequence of the chapters is logical, almost always leading to distinct synthesis. Properly it is a critical commented survey of many opinions — Takhtajan being clearly in complete command of the huge literature on the subject — but from which the author follows his own line of choice and judgement, accepting or rejecting with brief but clear comments. The whole argumentation is admirably concise and rouses admiration for covering this vast subject, comprising taxonomy, plant distribution, morphology, palynology, genetics, population dynamics, flower biology, anatomy, paleozoology, etc. Major questions are embodied in subsequent paragraphs: polyphyletism is rejected; ancestors must be sought among heterosporous ferns or fern-like plants followed by pteridosperms and certain gymnosperms, although direct ancestors cannot be indicated; the basal flower type of angiosperms was bisexual. Takhtajan attaches great importance to occurrence of plants in small populations, especially in mountain plants, facilitating chance variations and genetic drift, rapid spread of mutant genes, which is important for evolution. This entails that missing links are almost never fossilized. Micro-evolution is equalized with macro-evolution. Neoteny (on which Takhtajan devoted a former work) can lead to despecialisation through which phenotypic simplification the complexity of the genome remains intact; it may provide for a maximum phenotypic effect by a minimal genotypic change. Primitive wood structure of early Winteraceous angiosperms is understandable by neotenic origin. Evolution of angiosperms was not only rapid, but also discontinuous as a result of neoteny. Developing in the mountains ‘in many ..... small ..... populations ..... the earliest angiosperms found themselves under conditions most favourable to evolutionary radiation. And if we bear in mind that their evolution was closely tied to the evolution of insects and was based on the complex and peculiar mechanism of mutual selection, then the extraordinary speed of their initial differentiation becomes even more readily understandable.’ Protection of the ovules arose as a selection against damage by ‘early pollinating insects’; this made simplification of their structure possible which led to smaller ovules (loss of thickened integuments, sclerotesta, etc.) and enabled the angiosperms to observe the greatest economy of material in construction of the ovules and ♀ gametophyte, and it also made possible the perfection of the process of pollination. ‘The acquisition of the stigma was undoubtedly a very great event in the evolutionary history of seedplants.’ ‘The primitive insects searched for pollen (beetles), nectar searching ones were a further perfection; this again led to a very great advance in cross-pollination; and as a corollary to a greatly increased rate of evolution, which still continues.’ ‘Isolation of a population is well known to be a prelude to the formation of a new species.’ The question of the hypothetical reconstruction of the first flowering plants is approached by the ‘hypothetico-deductive method’. Knowing the basic evolutionary pathways of angiosperms and the main lines of specialisation of their organs and tissues, we may by extrapolation extend these lines mentally into the past to the lowest possible level of specialisation’, but somewhat further on he writes ‘This reconstruction of the ancestors of the living angiosperms depends on the truth of the assumption that they combined in one plant all the most archaic characters that are now found distributed among the living fossils.’ I have italicized in the citations two words that are in contradiction; furthermore I would like to point out that whereas each plant we know possesses both primitive and derived characters, we cannot make an exception for an ancestral plant; one which would contain all the archaic characters must logically be an idealized fiction.

Description: Rumphius (Herb. Amboin. 3, 1743, 19, t. 7) was the first to use the name Metrosideros, but of the 6 species he listed only the first, M. vera, belongs to the Myrtaceae. The same species is assumed to be the basis of Nani Adanson (Adanson, Families des Plantes 2, 1763, 88). Adanson did not list any species, but the assumption is based on the description and the fact that Rumphius had given the vernacular name of his Metrosideros vera as ‘Nani tree’.

Description: There are only two genera of the Aristolochiaceae, Aristolochia and Thottea, so far known to occur in Malesia. In the course of a revision of this family for the Flora Malesiana, some new species of both genera have been found. Eight new ones of Thottea were published in a precursor on that genus (Blumea 27, 1981, 301-332, f. 1-72). There are four new species of Aristolochia from Borneo and one more new Thottea from Sumatra to be described here.

Description: The pollen morphology of 18 out of 22 species of the genus Lepisanthes, as recently revised, was studied. General pollen morphology is rather uniform, but taxonomically significant differences exist in shape, relative length of ektoapertures, endoaperture development, and in the sculpture of the tectum. Detailed descriptions are presented and special attention is given to intraspecific variability. 10 Pollen types are recognized, most of which are linked by transitions. Morphological trends are established and the extent to which they indicate natural relationships is evaluated. In subgenera Lepisanthes and Erioglossum a less evolved but more variable pollen morphology is present, while in subgenera Otophora and Aphania derived pollen types occur, which agrees well with macromorphological evidence. Subgenus Erioglossum appears pollenmorphologically closely related to subgenus Lepisanthes. Subgenus Aphania can, both macro- and pollenmorphologically, be derived from subgenus Otophora. Within Lepisanthes tetraphylla close parallels exist between macromorphological and palynological interpretations of natural affinities between the numerous races. Lepisanthes fruticosa, in contrast, shows on both counts rather wide and continuous intraspecific variability. Also in Lepisanthes senegalensis continuous pollenmorphological variability is present, but here a clinal pattern can be detected. In general, geographically isolated or endemic forms in Lepisanthes show a tendency to develop deviating pollen types.

Description: Only two species of Gastonia occur in Malesia, but each has a complex taxonomie history. The species which became known first, G. papuana Miq., is evidently an uncommon plant of coastal and lowland forest, but with a very wide range. It has been collected only once, or at most a few times, from each of many islands of the Malayan Archipelago and once from the mainland of the Peninsula. Most of these collections were made in the nineteenth or early twentieth centuries. Only in western New Guinea has this species been collected in more recent times within our area. The distribution of this species shows several disjunctions, the most striking being that between West Irian and its only known locality in the extreme east of the Solomon Islands. It is interesting that this gap corresponds with the distributional range of the second species, G. spectabilis (Harms) Philipson, which overlaps that of G. papuana only in the west of New Guinea (fig. 1). The widely dispersed range of G. papuana has resulted in its being described as several distinct species from different parts of its range. It was first named in 1863, when three names appeared in two genera. Miquel (1863) applied the names Tetraplasandra paucidens and Gastonia papuana to this species, and Teysmann and Binnendijk (1863) described it as Tetraplasandra eupteronoides. I am grateful to Professor van Steenis for information on the sequence of publication of these names. Miquel’s publication was issued on 2 July 1863 (Stafleu, 1967). A report in volume 27 of the ‘Natuurkundig Tijdschrift voor Nederlandsch Indië’ states that volume 25 was issued in six instalments, the first of which appeared in 1862. The five remaining parts appeared in 1863. Professor van Steenis has examined the publication and concludes that page 416, on which the name T. eupteronoides appeared, belongs to the final instalment, and must therefore have been issued late in 1863, and in any event later than July. For this reason, Miquel’s names take precedence over that of Teysmann & Binnendijk. Of Miquel’s two names, I have chosen to use that which he placed in Gastonia. In this way the need for a new combination is avoided. As can be seen from its synonymy this species was described from other islands by subsequent authors.

Description: These fascicles, the first part of a moss flora of Fennoscandia, comprise five (acrocarpous) orders of the Eubryales. All species and a number of forms and varieties have been included. There are clear dichotomous keys to genera and species. Of each species the original literature, the most familiar synonyms, an excellent description with critical remarks on the differences between allied species and original drawings have been given. Ecology and general distribution have been indicated, with special reference to Scandinavia. In addition there is a glossary of technical terms, which is nearly identical to that in Dixon’s famous Student’s Handbook of British Mosses, though less extensive. Nevertheless it may be doubted whether this book actually fills a need in Scandinavian bryology. It is not suited for “workers in all fields of botany, forestry, limnology, etc.”, as the author suggests, since keys to the families are lacking. Besides, there is the excellent moss flora of Brotherus, Die Laubmoose Fennoscandias, not mentioned in this connection in the preface.

Description: In continuation of a former study on the ‘Elevation Effect’ in the Swiss mountain flora (Backhuys, 1968), the distribution of six Taraxacum species in Switzerland was examined in detail. This was enabled by the preceding monographic study by J. L. van Soest (1969). The interesting point was to compare species of one genus with a common dispersal mechanism. Data on the vertical distribution are provided in table I and diagrams 1—6. It was found that all six species show an elevation effect which varies from 200—750 m. In five species this range is as narrow as 500—750 m. See table II. It is concluded that in spite of the very obvious dispersal mechanism (parachute-achenes) the species are apparently not capable to colonise ‘mountain islands’ the summit altitude of which is situated between the lowest known locality and the lowest mountain island on which the species concerned is found. These data support the view that the elevation effect is a plant-geographical rule of universal validity for mountain plants.

Description: Carpels develop centripetally as oblique slightly ascidiform structures provided with a seat-like support. The terminal mouth of the ascidiform primordium becomes the lateral cleft of the carpel. Solitary terminal carpels develop as lateral structures. The sections Tasmannia and Drimys of the genus Drimys differ by the varying degree of ascidiform development. Austrobaileya is like Drimys. The structure of the carpel margins with submarginal placentation may have evolved from a slit like that in Winteraceae. Allometric development of an oblique ascidiform structure may have formed a large basal ovary, and may thus have moved the stigmatic part apically. A possible cupular origin of carpels is discussed.

Description: Trifolium repens has been introduced purposely or casually in the mountains of Luzon and East Java; it has now also turned up in New Guinea. EAST NEW GUINEA. Morobe Dist., Wau Subdist., Edie Creek, bank over gold workings, growing in profusion, NGF 12152 A. N. Millar, 14 Aug. 1968.

Description: Dispela ripot i toktok long wok bilong Dr C. Kalkman na Mr W. Vink, bilong Rijksherbarium long Leiden, Holland, wantaim Mr A. N. Gillison na Mr D. G. Frodin bilong Division bilong wok long Botany, long Lae. Oli bin mekim dispela wok long yar 1966 long ol dispela pies klostu long Tari: mauden Ambua, mauden Ne, mauden Kerewa na wanpela pies istap namel oli kolim Ibiwara. Oli bungim ol plaua, ol lip bilong diwai na ol diwai; olgeta samting em oli bungim wantaim inap long 1,975. Bihain, bai oli salim ol dispela samting igo long ol masta long university or bigpela skul we oli wokim wanpela buk oli kolim Flora. Dispela ripot bai toksave long ol kain diwai i stap long bus na ol kain plaua antap long mauden. Ripot ia i pinisim lukluk long plaua, long lain oli kolim Ericaceae i stap long ol dispela ples na antap long mauden Giluwe, mauden Kubor na mauden Wilhelm. Mipela i laik tok tenkyu long ol pipal bilong Tigibi na Benaria em oli bin wok wantaim mipela.

Description: The present paper deals with some gomphids from South America. Besides descriptions of a number of new species additional notes on several Selysian and other, little-known species, elucidated with illustrations of important details, are offered in order to obtain a better insight into the characteristics of these dragonflies. Lectotypes are selected and confusions in respect to the generic or specific status of some species are unraveled. Of nearly all the gomphids from Surinam the larval stages are described or discussed. The identity of several larvae is ascertained by the actual rearing of some individuals. The discovery of two new Agriogomphine species resulted in a classification of the members of the Agriogomphus complex into two genera only instead of four. Undoubtedly of greater importance is the attempt to acquire a satisfactory division of the large genus Gomphoides sensu Selysi 1854. In doing so, the erection of a new genus was necessary. The material from Surinam here recorded has been assembled in the first instance by the author himself during a period of ten years of odonatological research carried out in that country (1955—1965), but a comprehensive and very valuable part is from Dr. D. C. GEIJSKES. I would like to express here my thanks for his consent to describe his gomphid material. This privilege enabled me to clear up several intriguing problems on the regional gomphid fauna.

Description: The buthid scorpions of the genus Centruroides are widely distributed in the Antillean area. They are also the most common scorpions in the majority of these islands. Nevertheless they remained almost forgotten until recently (STAHNKE 1970; ARMAS 1976, 1977, 1980, 1981, 1982; FRANCKE & SISSOM 1980). For the purpose of this paper the Lesser Antilles are defined as the islands situated between the Virgin Islands and Trinidad & Tobago, according to BOND’S 1978 zoogeographical point of view.

Description: In the Netherlands Antilles, opposite the Venezuelan coast, the cyprinodont fish Poecilia sphenops vandepolli is found in fresh water, in brackish water, in the sea and in supersaline water. When comparing the populations from fresh water, sea water and supersaline water some significant morphological differences were found, e.g. in size, in depth of the body and of the caudal peduncle, in length of the head, and in the number of rays in the pectoral and caudal fins and the number of lateral scales. In raising experiments, however, it could be shown that these differences are phenotypic. The characteristics of the subspecies or varietas arubensis as described by VAN LIDTH DE JEUDE (1887) proved also to be phenotypic. Optimum growth was found in seawater. The adaptation to fresh water after transfer from sea water or supersaline water is quicker than in the opposite direction; this concerns specific weight adaptation, growth resumption and the change of preference for the new salinity after transfer. With respect to these characteristics fresh water is more favourable than sea water or brine. The inland migration after rainfall is not caused by the fresh water itself, but by an organic compound that is found in inland water, whether fresh or saline, and also in rain water after it has been in contact with the soil. From the fact that mollies also are attracted by IJsselmeer water, just as elvers are, it seems likely that mollies and elvers are attracted by the same organic compound. This behaviour of the molly causes irregular migrations from sea to inland waters which prevent the inland populations from developing into separate forms, races or subspecies.

Description: During the Late Devonian, deposition in the Cantabrian Mountains was largely controlled by movements along faults. By way of intermitting subsidence of the area south of the Sabero-Gordón line and the connected progradation of the coast during the Frasnian and early Famennian, three regressive sequences were deposited. On account of these sequences the Nocedo Formation is divided into three units. Before the late Famennian transgression, after which the upper part of the Ermita Formation was deposited, the area was peneplained. Six facies maps show the changes in palaeogeography during the Late Devonian.

Description: The investigated polymetamorphic peridotites occur associated with metabasic rocks in several complexes of probably Precambrian age in the northern part of the Hesperian massif (Iberian peninsula). Spinel-clinopyroxene-, spinel-pargasite-, spinel-hornblende- and chlorite-amphibole-peridotites, wehrlites, spinel-amphiboleand plagioclase wehrlites are found; most rocks are partly to completely serpentinized. Attention has been paid particularly to the two first-mentioned catazonal types in which bands, veins and lenses of garnet ± spinel pyroxenite and -pargasitite occur, while brown ceylonite orthopyroxenite and spinel-sensu-stricto clinopyroxenite are present in subordinate amounts. It is contended that these pyroxenites and pargasitites represent partial melting products of a parental ultramafic rock which contention is corroborated by experimental evidence. The partial melt had a picritic composition and crystallized as an aluminous pyroxene assemblage, in which garnet was formed under subsolidus conditions. Comparisons are drawn with peridotites from other occurrences in which garnet-bearing assemblages are also encountered. It is assumed that these peridotites were emplaced as spinel-clinopyroxene peridotites (Iherzolites) during a Precambrian orogenic cycle under high-pressure granulitefacies conditions and equilibrated at 1100°-1200°C under 15-20 kb pressure. Catazonal retrogradation (800°-900°C, 10-15 kb pressure) gave rise to large-scale development of pargasite. Garnet probably metastably coexisted with pargasite and the zonary character in the garnets was presumably obtained during this phase. Aluminous chlorite was formed during the Hercynian orogeny under mesozonal conditions; a second generation of pyroxenes and amphiboles possesses lower contents of Al2O3. The spinel-hornblende peridotite probably did not undergo high-pressure granulite-facies conditions during the Precambrian orogeny. The chlorite-amphibole peridotite is supposed to have a lower Paleozoic age. The wehrlites are considered to be partial melting products of a parental peridotite and crystallized under low pressures. Spinel-amphibole wehrlites are hydrated plagioclase wehrlites. New whole-rock analyses of 11 peridotites and 14 pyroxenites are given. Contents of some minor and some trace elements have been determined with neutron activation analysis. Electron microprobe analyses are presented of olivines, pyroxenes, amphiboles, garnets, spinels, chlorites, högbomites and ilmenites. The mineral compositions are compared to whole-rock chemistry and distribution coefficients are calculated from which temperature and pressure estimates are derived.

Description: The northern part of the contact aureole of the biotite-granite of Quérigut contains limestones and dolomites, which have been metamorphosed over a distance of about 100 to 150 metres. Further, a wide innermost border zone of the igneous body is characterized by the development of some hornblende and the occurrence of many dark inclusions, as well as aplitic and porphyritic dikes. A narrow outermost border zone of the granite is conspicuous by a much larger proportion of hornblende and accessories, the development of clinopyroxene in the immediate vicinity of the contact, and finally by a heterogeneous texture. Scarce localities where comparatively fresh granite is in direct contact with the dolomitic country rock, revealed the presence of a narrow zone of silicate skarn, developed exactly at the junction. Adjoining the skarn, the granite of the outermost border zone shows a very narrow and highly modified border facies over a distance of a few mm. to 5 cm., the so-called transition zone. Three types of this zone are distinguished: a prehnite-rich type, a clinozoisite- and zoisite-rich type and a grossularbearing one. Though the contact is very irregular, the zone of the silicate skarns follows all its curves and is remarkably constant in width (4—7 cm.). The adjoining country rock being almost pure dolomitic marble, the zone of the silicate skarns has apparently been formed by extensive metasomatism over a very limited distance. Within the skarn zone itself, a zonal structure is also apparent, with six different mineral assemblages, the spinel-xanthophyllite zone being the most conspicuous. Since the skarn consists mainly of a diopsidic clinopyroxene, it is broadly speaking a silicated dolomite. According to the mineralogical composition of the different zones, however, a certain amount of iron and aluminium has also been introduced by diffusion from the adjacent granitic magma, the proportion of both elements diminishing towards the marble. Among the various earlier and later minerals observed in the skarns, a thulite-like clinozoisite, amesite and diaspore may also be mentioned. Alternating layers of pure and impure limestones and dolomites, making up the bulk of the country rock, have been subjected to thermal metamorphism and partly also to pneumatolytic action. The pure limestones and dolomites were recrystallized to pure marbles. Impure limestones were transformed into calcite marbles with varying proportion of contact minerals, such as clinozoisite-epidote, prehnite, diopside, grossular, idocrase and wollastonite. Pure and impure quartzitic layers and lenses intercalated between the earlier limestones are now calc-silicate hornfelses, composed mainly of the minerals just mentioned. The impure dolomites were converted into dolomitic marbles with magnesium-rich minerals such as forsterite, phlogopite and spinel, while pneumatolytic action superimposed on the thermal metamorphism partly transformed the forsterite into clinohumite. Besides these four widespread minerals, chondrodite, humite and fluoborite have been found locally. Some of the spinels display two different colours within the same crystal. All steps in the progressive alteration of spinel into hydrotalcite are visible. Of the more than sixty minerals encountered in the rocks of the contact aureole and the border zone of the granite (listed on p. 255), six are probably new for France, viz. amesite, fluoborite, hydrotalcite, manasseite, xanthophyllite and a thulite-like clinozoisite. The alteration phenomena of some of the earlier minerals are of special interest and we may mention here that of spinel into diaspore, hydrotalcite and two types of amesite; of xanthophyllite into a. o. amesite, prehnite and clinozoisite; and finally of biotite into a. o. pumpellyite and garnet. Comparative studies of rocks from several other areas revealed similar alteration phenomena. The secondary garnet of a peculiar, flat, lenticular shape is probably of hydrothermal origin and appears to be a quite common mineral which has apparently hitherto been confused with other minerals such as zoisite. Finally, two new localities of clintonite have been found, one in Spain (Serranía de Ronda) and the other in the U.S.A. (Franklin).

Description: The area described comprises the SE plunging extension of the anticlinorium of Mondoñedo-Lugo-Sarria and several structural units to the NE of it. The stratigraphy compares with that of neighbouring areas. Certain new observations have been made regarding the west flank of the East Galician-West Asturian miogeosyncline at the end of the Precambrium and during the Early Palaeozoic. Stromatolites or algae played an important part in the formation of carbonate deposits during late Precambrian (Cándana limestone) and Lower Cambrian time (Vegadeo limestone). An imprint, possibly attributable to a specimen belonging to the Precambrian Ediacara fauna, was found in the Cándana Schist Formation. A shallow or relatively high zone existed during that time in the region around Incio. The same general area formed a high again at the end of the Ordovician, causing erosion and a marked disconformity of the Silurian. The Hercynian structures can be explained by assuming roughly WSW-ENE compression and shortening. In the NW of the area this is expressed in the first place by the recumbent folds of the Lugo-Sarria anticlinorium, and in the SE by the narrowness of the steep folds and their slightly changed direction in the general area of Seoane and El Cebrero. Normal crossfaults are related to the folding and the compression. They show locally a deviation in accordance with the direction of shear stress. Horizontal displacement along such faults in an EW direction was probably of little importance. Finally a few observations are given on the occurrence of Pb-Zn ores at the mine of Rubiales.

Description: Species of the heteropod families Carinariidae and Pterotracheidae collected in the Mid North Atlantic Ocean in 1980 have been studied. The distribution of the species is given, as well as the morphological variation. It is concluded that two subspecies of Carinaria lamarcki actually have to be considered distinctly recognisable and sympatric species, to be called C. lamarcki and C. challengeri. The vertical distribution of the heteropods studied proves not to be restricted to the photic zone and diurnal vertical migration occurs among the larger species. The horizontal distribution of the two Carinaria species and of at least two populations of the Pterotrachea species coincides with the southern branch of the North Atlantic Current, while others are restricted to the subtropical waters. Consequently, the present heteropods have to be considered good indicators of water masses and currents.

Description: Examination of the type specimens of Callichthys splendens Castelnau, 1855, Brochis coeruleus Cope, 1872 (type species of Brochis Cope, 1872), Brochis dipterus Cope, 1872, Corydoras semiscutatus Cope, 1872, Chaenothorax bicarinatus Cope, 1878 (type species of Chaenothorax Cope, 1878), and Chaenothorax eigenmanni Ellis, 1913, has demonstrated that they represent only one species: Brochis splendens. Callichthys taiosh Castelnau, 1855, also has to be considered a synonym of Brochis splendens. Chaenothorax multiradiatus Orcés-Villagomez, 1960, is a second species belonging to the genus Brochis.

Description: The bat fauna of the Adriatic islands is very poorly known in comparison with that of the coastal continental regions (Kolombatović, 1882, 1884; Dulić, 1959). Although ten species of bats are recorded, the data for most of the islands except the island of Lastovo (Dulić, 1968) are scarce, and of an early date. During the years 1966—1970, mostly in the summer (July, August), we investigated the bat fauna of some Adriatic islands, particularly of the southern ones. During 17 trips, each of 5 to 10 days, to 8 islands, 200 bats were collected and several hundreds were examined (caught in mist nets or taken in caves). The investigated area is shown in fig. 1, the distribution of the bats in table I. Bibliographical data included, 16 species of bats from the Adriatic islands (north, middle, and south) are known now.

Description: Moult cycle and morphogenesis in larval instars (zoea I, zoea II, megalopa) of the spider crab Hyas araneus were studied in the laboratory. Changes in the epidermis and cuticle were documented photographically at daily intervals to characterize the stages of the moult cycle. Stage A (early postmoult) is a very short period during which the larva takes up water. During late postmoult (B) and intermoult (C) the endocuticle is secreted, and there is conspicuous epidermal tissue condensation and growth. The onset of early premoult (D sub(0)) is characterized by epidermal apolysis, occurring first at the bases of the setae in the telson of zoeal instars or in the rostrum of the megalopa.

Description: Larval and early post-larval growth has been investigated in H. araneus L. (Majidae) reared in the laboratory. Growth was measured as dry weight (DW), ash-free dry weight (AFDW), carbon (C), nitrogen (N), hydrogen (H), gross biochemical constituents (protein, lipid, carbohydrate, chitin, ash) and energy (calculated separately from carbon and biochemical composition). During larval development, i.e. from freshly hatched zoea-I to late megalopa, all these criteria of biomass increase by factors ranging between 5 and 14; carbohydrate shows the lowest, chitin the highest increment. There are indications of loss in organic body weight during the latest period preceding metamorphosis to the crab stage. When no food is offered during this time, megalopae lose significantly more biomass than control larvae. This suggests that food is still required, but feeding activity is reduced to a level below maintenance ingestion rate. Following metamorphosis, the juvenile crab accumulates biomass at a far higher absolute rate (expressed as µg/d) than all larval stages.

Description: The development of hard bottom communities has been studied on test panels in Helgoland Harbour (German Bight) since 1977. Settlement and growth of epibenthic species was examined monthly. Natural variation in different seasons, years, and at three stations (the latter, only in 1981 and 1982) was investigated. At Station A (Binnenhafen), barnacles (Balanus crenatus ) and polychaetes (Polydora ciliata ) were always among the first settlers in spring. They were followed by other barnacles (Elminius modestus, Balanus improvisus ) and by colonical ascidians (Botryllus schlosseri ). The latter species often dominated from August to October, and tended to overgrow the barnacle populations.

Description: The larval development f the spider crab Hyas araneus L. was studied in the laboratory at different constant temperatures (2,6,12, and 18 °C). Linear relationships between log temperature and log stage duration were described by means of regression equations. They were used in a simple simulation model predicting larval moulting and metamorphosis at different temperatures. The most important predictions were : (1) Settlement of H. araneus takes place mainly from late May to mid-June; (2) assuming wide annual fluctuations in the average spring temperature ( plus or minus 2 °C), a total settlement period ranging from late April to early July can be expected; (3) delay of larval development due to a decrease in temperature is stronger than the acceleration caused by an equally great increase; and (4) both delay and acceleration effects become weaker during the hatching season and from stage to stage.

Description: Zoea-1 larvae of H. araneus were kept under different nutritional conditions. Their midgut glands were investigated with a transmission electron microscope. The glandular epithelium consists of the cell types known from adult decapods. It is mainly the R-cell type that undergoes ultrastructural alterations which reflect nutritional conditions. R-cells of fed larvae are characterized by large lipid inclusions; after a certain period of food deprivation (point-of-no-return) the original ultrastructure cannot be reestablished. Refeeding results in large glycogen deposits in these cells.