ALBERT

Description: https://www.researchgate.net/publication/230891291_The_Orbital_Theory_of_Pleistocene_Climate_Support_frim_a_Revised_Chronology_of_the_Marine_d18O_Record

Description: Summary Holocene sediments of the North Lagoon, Bermuda, were studied with shallow seismic reflection profiles (200 km CSP-survey, UNIBOOM-system) and vibration coring (40 sediment cores, pneumatic vibration corer, Meischner et al., 1981). Seismic Stratigraphy Four seismic sequences are distinguishable by seismic stratigraphy. All seismic sequences correspond to depositional sequences built up during high sea levels in interglacial times. The seismic sequences are separated by unconformities which are often strongly reflective and correspond to emersion planes during glacial phases. The upper sequence (sequence 4) is related to Holocene sediments. The pre-Holocene bedrock is divided into three different seismic sequences (Kuhn et al., 1981): Sequence 1: oldest Pleistocene sequence (pre-Sangamon sea-level highstands), upper boundary with levelled relief (lower boundary not discernible), composed of strongly cemented carbonate sediments, forms the bedrock below Three Hill Shoals Sequence 2: Sangamon (125 ky sea-level highstand), distinct surface morphology, forms the bedrock of a large area below Holocene sediments, Holocene reefs grew up on elevations of the sequence 2 surface, the Holocene reef rim was developed on an elevated rim of sequence 2 Sequence 3: youngest Pleistocene sequence (Sangamon, 105 and 85 ky sealevel highstands lower than recent), deposited mainly in depressions of the bedrock deeper than -15 m below recent Mean Sea Level, levelling the older relief, peat sedimentation in places The distribution of recent reef areas and lagoonal basins is strongly controlled by pre-Holocene topography and geology of the bedrock. During the Holocene approx. 1050 x 106 m3 of carbonate sediments were deposited in the North Lagoon (290 km2) and approx. 1350 x 106 m3 in the reef rim area (170 km2). Sedimentology There are no larger oscillations of the Holocene sea level identifiable in the sedimentological record. The pre-Holocene topography was gradually drowned during the Holocene sea-level rise. At first, the depositional depressions were separated and landlocked. Fresh water peat marshes, fresh water ponds, marine ponds and bays were formed. With rising sea level, the land barriers were more and more eroded, drowned and lost their influence on the back-barrier sedimentation area. Autochthonous and allochthonous peat, lime gyttja and carbonate mud are a typical transgressive back-barrier sediment sequence. After destruction of the barrier, the depositional milieu changed from restricted marine to normal marine, open lagoonal. Sea-grass sediments and nearly mud-free carbonate sand were deposited in shallow water in an exposed environment. Hydrodynamic energy decreases with increasing water depth in the lagoonal basin. A more densely growing reef rim and intralagoonal reef growth added to the protection of the deeper lagoonal floors. Fine-grained sediments were deposited in this environment. They are distributed over a large area of the North Lagoon and form the top of the transgressive lagoonal sediment sequence. Holocene reefs mainly developed on rises of the pre-Holocene surface. In the early Holocene, solid reef build-ups were able to keep up with the rapid rise of sea level. Sand pockets in the reefs were left behind and filled up mainly in the later Holocene. The percentage of fine-grained sediments, produced and resuspended in the reef rim and deposited in the near lagoonal back-reef zone, increased during the Holocene. Two models of Holocene sedimentation in a depression and on an elevation of the pre-Holocene surface illustrate the dependence of vertical facies gradation on pre-Holocene topography. Trends of the mostly polymodal grain-size distributions of the Holocene sediments are a coarsening-upward in the back-barrier and a fining-upward in the lagoonal sediment sequences. Change in the composition of the molluscan fauna in the Holocene sediments (particle size 〉 2000 µm) is an Indication for fades changes. Gastropods are abundant in the basal backbarrier sediments. Bivalves are rare and their diversity 1s low. Sea-grass sediments contain Codakia orbicularis and Astraea phoebia shells. In the sheltered lagoonal environment shell fragments 〉 2000 µm become rare, common species are Gouldia cerina, Pitar fulminata and Finella sp. (approx. 1000 µm). Fine-grained reef-rim derived sediments differ from lagoonal sediments by a higher percentage of Homotrema rubrum fragments and Alcyonaria spicules.

Description: Verslag van een doctoraal onderwerp bij de Vakgroep Systematische Dierkunde en Evolutiebiologie van de Rijksuniversiteit Leiden, september 1976

Description: Op 27 mei 1976 overleed Dr. P.A. Florsohütz op de leeftijd van 53 jaar. Het bericht van zijn overlijden kwam zelfs voor diegenen die gedurende de laatste weken van zijn leven regelmatig kontakt met hem hadden onverwacht. Tijdens de middelbare-sohooltijd kwam zijn interesse in de biologie al duidelijk naar voren. Zowel plant als dier had zijn belangstelling. Na het behalen van het diploma HBS liet Florsohütz zich als student in de biologie aan onze universiteit in schrijven en legde in 1945 bet kandidaatsexamen af. Spoedig daama werd hij kandidaat-assistent bij Prof. Pulle, hoogleraar-directeur van het toenmalige Botanisch Museum en Herbarium. Hét doctoraal-examen werd in 1949 afgelegd.

Description: Floristische und soziologische Beobachtungen über die Flechtenvegetation von Isla Persa, einer Gletscherinsel in der SO-Schweiz (Berainagebiet), in Höhe von 2450-2850 m, werden beschrieben. Die Artenliste nennt 156 Arten. Die interessantesten Funde werden kurz besprochen. Deutlich höher als bekannt aus der Literatur wurden gefunden: Cladonia cyanipes auf 2550 m. Coniocybe furfuracea auf 2650 m. Leprocaulon microscopicum auf 2500 m. Weiter werden einige Flechtengesellschaften auf Isla Persa kurz besprochen: a) epiphytisch: Parmeliopsidetum ambiguae Hilitzer 1925 b) epilithisch: Umbilicarietum cylindricae Frey 1923 Umbilicarietum microphyllae Frey 1923 Sporastatietum testudineae Frey 1922 Sporastatietum polysporae Frey 1922 Ramalinetum capitatae Frey 1923 Umbilicarietum ruebelianae Frey 1925 Dimelaenetum oreinae Frey 1923 Umbilicarietum deustae Frey 1933 c) terrestrisch: Stereocauletum alpini Frey 1937 ? Cladonietum alpestris Frey 1937 Thamnolietum vermicularis Gams 1927 Lecideetum demissae Frey 1923

Description: The African members of the Conocephaloideae are revised. Musanga comprises two species: M. cecropioides and M. leo-errerae. In Myrianthus seven species are recognized: M. arboreus, M. holstii, M. preussii (with ssp. preussii and ssp. seretii), M. libericus, M. serratus (with var. serratus and var. letestui), and M. cuneifolius. M. serratus var. letestui is described as new.

Description: The first record of Lophozia perssonii for the Netherlands, from an old and deep limestone-quarry near Cadier en Keer, S. Limburg. Sterile L. perssonii grows here as a pioneer on shaded, calcareous tufa blocks together with Leiocolea badensis and other bryophytes. The differences with related species are discussed, and a description of the ecology is given.

Description: The South Asia Institute (see note on page 2342) has changed its address in Heidelberg, Germany: now P.O. Box 10 30 66. Work is in progress on the geography – with a botanical inclination – on Nepal, Ceylon, Java, Sumba, Timor, Papua New Guinea, and Stewart Island, New Zealand. New policy of NUFFIC. The two projects executed by the Rijksherbarium for the Netherlands University Foundation For International Cooperation: seedlings in Bogor and Flora of Thailand, have been completed and discontinued respectively. Both were conceived in the early days of NUFFIC, when initiatives of interested parties were welcomed. Election of a socialist government in Holland in 1973 brought a gradual change in policy, towards larger, multidisciplinary projects for the benefit of the poorest, and we were informed that small projects like the above would not be accepted. We will see what the next elections bring, in 1977.

Description: Tabula Rasa. In 1963 as a missionary I arrived in the Flora Malesiana region, notably in the Lesser Sunda Islands. A certain ’sensus botanicus’ was my only equipment for botanical surveys, and the next thing to do was to walk the arduous but occasionally quite entertaining road to discovery. I often felt like Mr. Columbus when he was discovering America. I entered the New World at Port Said. A lovely ’pine avenue’ drew me, which turned out to consist of arborescent Equisetes! I now realize that it must have been Casuarina, and still these trees, which I grow in my garden are a source of delight to me. Later it was the tropical gardens with their ’unending splendor of flowers’ that captivated my interest, until one day I learnt that Canna indica is of American origin and that there is indeed a kind of commonplace tropical assortment. For meanwhile I had found occasion to set foot in a genuine Asian primary forest, where reality turned out to be a tedious green monotony. This ’dead point’ must perhaps be reached and passed by anyone who finds himself unprepared like me in the Malesian plant kingdom before, step by step, he can learn to know and love the true ’Flora Malesiana’.

Description: ANDERSON, J.A.R., A checklist of the trees of Sarawak, 364 pp. (1983, Dewan Bahasa dan Pustaka Cawangan Sarawak, for Forest Department, Kuching, Sarawak). Cloth Mal$ 15.00. When Dr. Anderson retired from the Forest Department in 1973 he left the manuscript of this checklist for publication. Unfortunately publication was delayed for 10 years. It contains data on over 2500 arboreous plant species. The text consists mainly of two parts: the first is a list of vernacular names with their scientific equivalents, the second is a list of plant names alphabetically arranged by family. Each species is concisely annotated with its vernacular name(s), maximum diameter, ecology, frequency, soils, etc. Species names have been coded: the first two figures are for the family, the next two for the genus and the last two for the species. A list is given of the trees of the peat-swamp forests of which Anderson was a great expert. A small draw-back is that the literature of the last ten years has not been included. Nevertheless this is a most helpful book. — C.G.G.J. van Steenis.

Description: Take almost any profile diagram of rain forest and it reveals you the neglect: nothing but trees. Even in Flora Malesiana* the manner of their climbing is not always indicated. Foresters regard them as weeds and persecute them systematically (see FOX 1968), which subjects them to extra dangers beyond the ’normal’ forest devastation. This makes them perhaps the most threatened life form amongst plants. Yet it is good to remember that two of the main climber families, Menispermaceae and Piperaceae, contain an extraordinary variety of interesting chemical substances (see HEGNAUER in the reference list). For this same reason it is risky to drink water from Menispermaceae trunks, as can be done by holding up a fresh-cut piece of 1-1½ m (Piperaceae are slenderer). Rattans, which are largely bound to primary forest, are of course well known, also economically. Horticulturists have taken hundreds of ornamental climbers in cultivation, on which MENNINGER produced a large popular book, with quite a body of practical knowledge. Lianas (i.e. the larger woody vines) occur in a great number of families, although concentrated in about a dozen; taxonomically as well as morphologically they are heterogeneous. They are a main feature of the tropical forests, where according to an old estimate, they make up 8% of the flora, far less so in the temperate forest (about 2% of a much poorer flora). MEIJER (quoted by FOX, 1968) estimated their number for Sabah alone at 150 genera: 13 in the Asclepiadaceae, 12 in the Menispermaceae, 10 in the Rubiaceae, 9 in the Apocynaceae, 9 in the Leguminosae, 8 in the Annonaceae. As for numbers of individuals, in Sabah, FOX (1969) found on ten plots of 0.4 hectares in typical lowland dipterocarp forest an average of 839 climbers (range 472-1146); out of these 690 (range 380-1003) were thinner than 2½ cm, while 56 (range 28-91) were thicker than 5 cm.

Description: Small evergreen trees, shrubs or lianas; two genera ( Cansjera and Opilia) are known to be root-parasites. Leaves distichous, simple, usually extremely variable in form and size, entire, exstipulate, pinnately veined; dried leaves mostly finely tubercled by cystoliths located in the mesophyll. Inflorescences axillary or cauliflorous, panicle-like, racemose, umbellate (in Africa) or spicate; bracts narrowly ovate or scale-like, in Opilia peltate, often early caducous. Flowers small, (3—) 4—5) (—6)-merous, mainly bisexual, sometimes unisexual and plants then dioecious ( Gjellerupia, Melientha, and Agonandra) or gynodioecious (Champereia). Perianth with valvate, free or sometimes partly united tepals (in ♀ flowers of Gjellerupia wanting). Stamens as many as and opposite to the tepals (in ♀ flowers only small staminodes); anthers introrse, 2-celled, longitudinally dehiscent. Disk intrastaminal, lobed (lobes alternating with the stamens), annular, or cupular. Ovary superior, 1-celled; style short or none, stigma entire or shallowly lobed. Ovule 1, pendulous from the apex of a central placenta, anatropous, unitegmic and tenuinucellar. Fruit drupaceous, pericarp rather thin, mesocarp ± fleshy-juicy, endocarp woody or crustaceous. Seed large, conform to the drupe, without testa; hilum basal, often in a funnel-shaped cavity. Embryo terete, embedded in rich, oily endosperm, nearly as long as the seed or shorter, with 3—4 linear cotyledons, radicle often very short. Distribution. There are 9 genera with about 30 spp., widespread in the tropics. Rhopalopilia is restricted to Africa and Madagascar, Agonandra to South and Central America. In Malesia: 7 genera, 5 of these only known from the eastern Old World (1 endemic: Gjellerupia in New Guinea); Opilia and Urobotrya occur also in tropical Africa.

Description: Monoecious, medium-sized to very large trees (rarely shrubby in very exposed situations). Either four independent cotyledons or two fused pairs (which may be retained in the seed after germination). The growing point of foliage shoots quite distinct between the two genera, being just a few highly reduced leaves in Araucaria and a highly organized bud formed of overlapping scales in Agathis. The leaves vary from scales or needles to broad leathery forms with many parallel veins sometimes on the same plant at different stages of growth. Pollen produced in cylindrical cones from one to as much as twenty cm long with numerous pedunculate spirally placed microsporophylls each with several to many pendent elongated pollen sacs attached to the lower side of an enlarged shieldlike apex which also projects apically more or less overlapping the adjacent microsporophylls. Pollen cones solitary, terminal or lateral, on branches separate from those bearing seed cones, subtended by a cluster of more or less modified leaves in the form of scales, deciduous when mature. Pollen globular, without ‘wings’. Seeds produced in large, well-formed cones which disintegrate when mature, dispensing the seeds in most cases with the help of wing-like structures; the seed cone terminal on a robust shoot or peduncle with more or less modified leaves that change in a brief transition zone at the base of the cone into cone bracts, formed of numerous spirally-placed bract complexes, usually maturing in the second year. Individual seed cone bract leathery or woody and fused with the fertile scale which bears one large inverted seed on its upper surface. Distribution. The 40 species in two genera are well represented in Malesia (13 spp.) and extend eastward and southward into Fiji, New Caledonia (18 spp.), Australia, and New Zealand, with 2 spp. also in the cooler parts of South America, giving the family a distinct Antarctic relationship. Only one species of Araucaria (in South America) occurs completely outside of the tropics, while the majority of the species in the family belong in the lowland tropics and others grow in the tropical highlands.

Description: Applied Ecology Abstracts, compiled and published by Information Retrieval Ltd. 1 Falconberg Court, London W1V 5FG, U.K. A monthly, each issue carrying c. 800 abstracts and author index. Price vol. 1, Jan.-Dec. 1975, surface mail £ 60, airmail £ 73. It is claimed that 4300 journals and other publications are scanned annually. Coverage is world-wide.

Description: Many botanists must have wondered why as yet no volume of Flora Malesiana was dedicated to the outstanding botanist Carl Ludwig Blume, undisputed pioneer in planning the compilation of a ‘Flora Malesiana’. The writing of this Dedication would have been greatly facilitated if a full biography of BLUME had been existent, but none is available; there is not even a bibliography of his works. Only recently, in 1979, two biographical attempts were made, by J. MACLEAN and by A. DEN OUDEN, but only for the period 1820-1832; together with other biographical and obituary notes they are here assembled in Appendix B. I have also compiled a bibliography: Appendix A.²

Description: Erect or straggling herbs, shrubs or trees, sometimes monoecious or dioecious, the herbs sometimes rhizomatous; branches sometimes jointed at the nodes, sometimes without vessels ( Sarcandra). Leaves simple, decussate or sometimes whorled in fours, serrate, crenate or dentate, the teeth often thickened at the apex, penninerved, usually petiolate; petioles more or less connected at the base at least by a transverse line or connate into a distinct sheath; in Ascarina often alternating with leafless internodes which have the petiolar sheath; stipules minute to fairly conspicuous, subulate, borne on the petiole bases or sheath, occasionally pectinate. Flowers much reduced, without perianth, fully unisexual or essentially bisexual with the reduced anther-bearing organ adnate to the side of the ovary; arranged in spicate, paniculate, or capitate axillary or terminal inflorescences. — Male flowers bracteate or not, apparently consisting of 1—5 stamens, or in Hedyosmum consisting of numerous anthers in a cone-like structure; if 3 then the whole forming a fused 3-lobed organ sometimes enveloping the female flower by its edges, the central anther with 2 or aborted loculi and the laterals with single loculi, simply lobed or with connectives slightly to considerably produced so that the whole organ is 3-fingered; if with only 2 anther locelli then these on either side of a thickened filament plus connective. — Female flowers naked or enclosed by a cupular bract, the perianth adnate to the ovary, often minutely or shortly dentate at the apex and the ovary thus inferior; ovary 1-locular; stigma sessile or style short; truncate, 2-lipped, depressed or subcapitate (or horseshoe-shaped in one species), rarely linear or clavate. Ovule solitary, orthotropous, pendulous, bitegmic and crassinucellate. Drupes fleshy, small, ovoid or globose, sometimes more or less 3-sided in Hedyosmum, free or united into a mass by the bracts; endocarp hardened and crustaceous. Seeds subglobose, exarillate, with copious fleshy or oily endosperm and minute embryo, the cotyledons divaricate or scarcely formed. Distribution. Four genera with about 80 species. Since VESTER’S (1940) small-scale map the family (Ascarina) has been found in Madagascar. It is mainly tropical but Ascarina extends south to North Island of New Zealand (fig. 6) and Chloranthus and Sarcandra extend north to Japan, China, Korea and the eastern U.S.S.R. (Ussuri).

Description: Trees or shrubs (or rarely suffrutices outside Malesia). Leaves simple, alternate, often coriaceous, glabrous or with an indumentum on undersurface, margin entire; petioles often with 2 lateral glands. Stipules 2, minute and caducous to large and persistent, usually linear-lanceolate. Inflorescence racemose, paniculate or cymose; flowers bracteate and usually bibracteolate; bracts and bracteoles small and caducous or larger and enclosing flower or groups of flowers and persistent. Flowers actinomorphic to zygomorphic, hermaphrodite or rarely polygamous, markedly perigynous. Receptacle campanulate to cylindrical or rarely flattened cupuliforum, often gibbous at base; calyx lobes 5, imbricate, often unequal, erect or reflexed. Petals 5 (absent in some Neotropical species), inserted on margin of disk, commonly unequal, imbricate, deciduous, rarely clawed. Stamens indefinite, 2—60 (to 300 in Neotropics), inserted on margin of the disk, in a complete circle or unilateral, all fertile or some without anthers and often reduced to small tooth-like staminodes; filaments filiform, free or ligulately connate, short and included to long and far exserted; anthers small, 2-locular, longitudinally dehiscent, glabrous or rarely pubescent. Ovary basically of three carpels but usually with only one developed, the other two aborted or vestigial, variously attached to (the base, middle or mouth of) receptacle, usually sessile or with short gynophore, pubescent or villous; ovary unilocular with two ovules or bilocular with one ovule in each locule. Ovules erect, with micropyle at base (epitropous). Style filiform, basally attached; stigma 3-lobed or truncate. Fruit a fleshy or dry drupe of varied size, interior often densely hairy; endocarp much varied, thick or thin, fibrous or bony, often with a special mechanism for seedling escape. Seed erect, exalbuminous, the testa membraneous; cotyledons amygdaloid, plano-convex, fleshy, sometimes ruminate. Germination hypogeal with the first leaves opposite or alternate or epigeal with opposite first leaves. An extensive review of the generic limits of the family has been published: G.T. PRANCE & F. WHITE, The genera of Chrysobalanaceae: a study in practical and theoretical taxonomy and its relevance to evolutionary biology, Phil. Trans. Roy. Soc. London 320 (1988) 1—184. This contains full details of taxonomic history, morphology, anatomy, pollen, ecology and distribution of the family. A condensed version of these subjects is given here. Details of the Neotropical members of the family are given in: G.T. PRANCE, Chrysobalanaceae, Flora Neotropica 9 (1972) 1—410. The African members of the family were treated in: F. WHITE, The taxonomy, ecology and chorology of African Chrysobalanaceae (excluding Acioa), Bull. Jard. Bot. Nat. Belg. 46 (1976) 265—350.

Description: Perennial herbs, more commonly woody at the base, undershrubs or shrubs, erect, scrambling or scandent, sometimes high lianas. Rhizome not rarely tuberous. Branches often slightly swollen and jointed at nodes. Hairs simple, uni- or multicellular, short ones often with a hooked apex. Leaves simple, spiral or alternate, petioled (without an abscission zone), exstipulate; midrib usually prominent beneath, elevated or flat above; nervation commonly palmate, or pinnate, nerves often obliquely extending towards the margin. Flowers bisexual, actinomorphic or zygomorphic, solitary, fasciculate, or in axillary or cauligerous, racemose, paniculate or cymose inflorescences, usually only one or two flowers open at a time; bracts present and often persistent; pedicel often hardly distinct from the ovary. Calyx petaloid, gamosepalous, 3- (or 6-) lobed or 1-lipped; lobes valvate or induplicate. Petals (in Mal.) absent. Disk (?) 0, rarely present (e.g. a few Thottea spp.). Stamens 6 (4 or 5 in some extra-Mal. Aristolochia spp.) or 6—c. 36 (—46), in 1 whorl or in 2 (3 or 4) whorls (Thottea); filaments free or slightly mutually united at the base, and/or almost completely adnate to the style column to form a gynostemium; anthers free (Thottea) or dorsally united with the style column (Aristolochia), each consisting of 2 thecae with 4 pollen sacs, extrorse, rarely introrse (extra-Mal. spp.), dehiscing longitudinally. Ovary inferior (rarely half-inferior in extra-Mal. genera), 4—6-carpellate, 4—6-celled, syncarpous (or ± apocarpous in extra-Mal. Saruma); placentae parietal (distinct when young, then intruding and connivent axially, thus often seemingly axile); ovules usually many, anatropous, in 1 or 2 vertical rows in each locule of the ovary, horizontal or pendulous; style-column 3—many-lobed, sometimes some of the lobes redivided; stigmas or stigmatic tissue apical, lateral, or on the surface of style lobes. Fruits capsular or siliquiform (follicular or cocci in extra- Mal. genera), 4—6-celled; dehiscing apically towards the base (basipetal, e.g. Thottea) or basally towards the apex (acropetal, e.g. most Aristolochia); septicidal, rarely septifragal (some extra-Mai. Aristolochia) or bursting irregularly (extra-Mal. Asarum); rarely indehiscent (W. African Pararistolochia). Seeds many in each locule (1-seeded in extra-Mal. Euglypha), often coated with remains of placental tissue (membranous when dry), horizontal or pendulous, variously shaped; ovate, deltoid or triangular, flat, convex-concave, or longitudinally curved, or oblong (and triangular in cross-section), rugose, finely verrucose, or smooth, immarginate (Thottea; Aristolochia, p.p.) or winged (Aristolochia, p.p.); albumen fleshy, copious; embryo minute, cotyledons two, distinct. Distribution. There are 7 genera, Aristolochia worldwide, Asarum over the northern hemisphere, Thottea in continental Southeast Asia and Malesia, Pararistolochia in tropical Africa, and 3 monotypic genera, viz. Saruma in China, Holostylis and Euglypha in South America. As to number of species, Aristolochia is by far the largest with some 300 spp., largely concentrated in the New World, especially in Central and South America, in Malesia with 28 spp.; Asarum (incl Hexastylis and Heterotropa) with possibly some 70 spp. in northern temperate regions, Thottea with 26 spp., of which 22 in Malesia, and Pararistolochia with 12 spp. in West Africa.

Description: Fungi producing ornamented asexual structures and belonging to the Oomycetes (Trachysphaera) or Zygomycetes (Azygozygum, Mortierella) are described. They were studied by light and scanning electron microscopy while also mating experiments and carbohydrate analyses were performed. Azygozygum chlamydosporum is closely related to Mortierella indohii and therefore Azygozygum is considered to be a synonym of Mortierella. Mortierella echinosphaera spec. nov. is also closely related, but no zygotes are known, only ornamented chlamydospores have been observed. Absence of glucuronic acid and fucose and a low glucosamine content in Trachysphaera fructigena show that it belongs to the Oomycetes.

Description: The genus Mycoacia Donk (1931) originally contained four species, viz. M. fuscoatra (Fr. ex Fr.) Donk (type), M. uda (Fr.) Donk, M. stenodon (Pers.) Donk, and M. setosa (Pers.) Donk. This last species, however, is the type species of Sarcodontia S. Schulzer 1866. Later (1952) Donk considered M. setosa as generically distinct. The monotypic genus Sarcodontia has globose to subglobose spores with thickened walls and is parasitic, while Mycoacia has ellipsoid to allantoid thin-walled spores and is saprophytic. When Mycoacia and Sarcodontia are considered as congeneric (e.g. Nikolajeva, 1961), Sarcodontia is the correct name for the genus. Mycoacia and Sarcodontia are both classified in the Corticiaceae (Donk, 1964; Parmasto, 1968); they are characterized by the resupinate hydnoid ceraceous basidiocarp, the monomitic hyphal system and the smooth non-amyloid spores. The genera are closely related to Phlebia.

Description: Type material of Tulasnella cystidiophora Höhn. & Litsch. has been studied. The species is characterized by often moniliform gloeocystidia and clamp-less hyphae (at least in the subhymenium).

Description: A new species, Alstonia undulifolia Kochummen & Wong, is described from the Malay Peninsula. Two sections of the genus occur in the Malay Peninsula, Alstonia sect. Monuraspermum Mon. and Alstonia sect. Alstonia, the latter being the correct name for what was previously known as sect. Pala (Adr. Juss.) Benth. Various characteristics, including growth architecture, are examined for their usefulness in distinguishing these two sections of the genus. In comparing A. angustiloba Miq. and A. pneumatophora Berger, both of which have not been properly differentiated by characteristics of the reproductive organs, A. pneumatophora var. petiolata Mon. is reduced to synonymy under A. angustiloba. A key to the seven species of Alstonia native to the Malay Peninsula is provided.

Description: In Malesian Sterculiaceae there was still one enigmatic monotypic genus unsolved, Leptonychiopsis (parviflora) Ridl., J. R. As. Soc. Str. Br. 82 (1920) 173; Fl. Mai. Pen. 1 (1922) 290, described after a specimen collected by a Malayan, 10 Dec. 1892, filed under Ridley 3743. Ridley distinguished this from Leptonychia by its 3-merous flowers. Recently I could borrow a type sheet from the Kew Herbarium to which is attached an ample pencil-drawn analysis. Unfortunately, it is hardly feasible to check this, as there is only one small bud on the specimen, which I did not dare to analyse.

Description: Revision of the Malesian species of the genus Steganthera, which centres in New Guinea; precursor to treatment in Flora Malesiana. There are 16 species accepted; 5 are described as new, 12 names are reduced, 3 are excluded and 9 are imperfectly known.

Description: In a recent thesis B.S. Fey (Zürich) has developed a new theory about the origin of the cupule in Fagaceae. He has concluded that the appendages (spines, lamellae, etc.) on the outside of the cupule are regularly arranged and that they reflect a condensation (concrescence) of a dichasial flower system, so that cupule and fruit(s) form together the representation of one ancestral inflorescence; the cupular appendages would then largely represent the bracts of the ancestral inflorescence. This stands in contrast with former opinions, in which the cupule was interpreted as of separate vegetative origin from the nut(s) which was (were) the remain (s) of the inflorescence.

Description: Recent studies in Sabah and Sarawak have demonstrated the presence of an undescribed species of Podocarpus.

Description: In a comprehensive treatment of Caltha, Petra Smit (Blumea 21: 119—150. 1973) unfortunately chose an incorrect name for her fourth variety under C. palustris L. Instead of var. radicans (Forst.) Beck, this taxon should be called C. palustris var. flabellifolia (Pursh) Torrey & Gray (Fl. N. Am. I: 27. 1838). Forster’s C. radicans was described in 1807 (Trans. Linn. Soc. 8: 324) and reduced to varietal status by Beck in 1886 (Verh. Zool. Bot. Gesellsch. Wien 36: 350). According to the current International Code of Botanical Nomenclature, no name has priority outside of its rank (cf. Art. 60). Inasmuch as C. palustris var. flabellifolia was the name first established for Smit’s variety d’, as such it has priority over C. palustris var. radicans (Forst.) Beck by 30 years.

Description: Pholidota kinabaluensis is transferred to the new monotypic genus Entomophobia. Coelogyne phaiostele, C. ridleyana, and Pholidota triloba are identical and transferred to the new genus Geesinkorchis, that also comprises the new species G. alaticallosa. The monotypic genus Sigmatochilus is reduced to Chelonistele, in which C. dentifera and C. lurida var. grandiflora are described as new. Chelonistele crassifolia is regarded as a variety of C. sulphurea.

Description: The genera Hunteria and Lepiniopsis of the family Apocynaceae are in Malesia represented by one species each. Distribution and ecology are cited in full.

Description: Five new species of Rafflesia (Rafflesiaceae) are described, while attention is drawn to a sixth, possibly also new one. A key to all recognized species is given.

Description: The morphology and leaf anatomy of Myxopyrum is described and a key to the species is given. Of the 15 species previously described four species and two subspecies are recognised: M. nervosum Bl. (synonyms M. horsfieldii, M. zippelii) with one subspecies coriaceum (Bl.) Kiew (synonym M. ellipticum), M. ovatum Hill (synonyms M. macrolobum, M. cordatum, M. philippinensis), M. pierrei Gagnep. (synonym M. hainanense) and M. smilacifolium Bl. (synonym M. serrulatum) with one subspecies confertum (Kerr) Kiew. Myxopyrum enerve Steen. is Chionanthus enerve (Steen.) Kiew. Descriptions for the extra-Malesian species, M. smilacifolium, is given.

Description: In subgenus Malachobatus twenty Malesian species are recognized, one of them ( Rubus moluccanus L.) with four varieties. Synonymy, descriptions, habitat notes, etc. are given. New names: R. moluccanus L. var. discolor (Bl.) Kalkm. and var. angulosus Kalkm. A key is given to the Malesian species.

Description: On 11 September 1976 dr. Reinier Cornelis Bakhuizen van den Brink will reach the age of 65 and so he must retire from his position as a senior botanist at the Rijksherbarium. He has worked in our institute since December 1943, after having obtained his doctor’s degree in Utrecht. At the Rijksherbarium he became heavily involved in the preparation of the so-called ‘emergency edition’ of C. A. Backer’s Beknopte Flora van Java, which was mimeographed during the war in order to restrict the chances of destroyal of Backer’s valuable manuscripts. When after the war it was decided to translate Backer’s concise flora into English and to update and complete it, he gradually took over the burden from Backer who in 1945 was already over seventy. As a consequence the Flora of Java, published in three parts between 1963 and 1968, bears both names as authors on the title-page. Quite appropriately too, seeing that he devoted so much of his time, energy, and knowledge to this piece of work.

Description: In Southeast Asia (excluding India) 44 taxa are recognized, 39 species, of which four are newly described ( I. kerrii, I. luzoniensis, I. emmae, and one unnamed species A, which will be treated by Nguyen Van Thuan, Paris), four subspecies, one of which is new (I. sootepensis subsp. acutifolia) and three are new combinations ( (I. suffruticosa subsp. guatemalensis, I. trifoliata subsp. unifoliata, I. trita subsp. scabra) ), and one variety which is a new combination I. spicata var. siamensis). A key, descriptions and full synonymy are given as well as 4 distribution maps and 5 figures.

Description: The factors influencing the development of brashness in timber are discussed. These are reduction in density; changes in moisture content and temperature; ultrastructural changes; changes in chemical composition; and the presence of compression damage. Examples are cited and illustrated. Attention is paid to the recognition of the causes of brashness in the field and in the laboratory.

Description: The duration of cambial activity, and change in wood structure from early to latewood, are considered in relation to the initiation of scale and foliage leaves, and shoot extension, in Picea abies, Pseudotsuga menziesii, Quercus robur, Fraxinus excelsior, and Fagus sylvatica. The initiation of cambial activity appears to be associated with the production of the first scales at the shoot apex, but the cessation of cambial activity does not appear to coincide with the end of primordial initiation at the apex. In P. abies and P. menziesii leaf initiation continues at a rapid rate for several weeks after cambial activity has ceased. In Q. robur, F. excelsior, and F. sylvatica cambial activity continues longer than leaf initiation. The decline in vessel or tracheid diameter is not consistently related to the change from initiation of scales to initiation of foliage leaves. In the ring porous hardwoods the rapid decline in vessel diameter at the end of the earlywood coincides with the cessation of shoot elongation, but in the other species vessel or tracheid diameter declines steadily from the beginning of the earlywood.

Description: A list is provided of the species, subspecies and synonyms of the tipulid genus Nephrotoma Meigen, 1803. The distribution of each species is given in subregional quotations.

Description: Variability in the anatomy of root wood of selected specimens particularly Fraxinus excelsior L. and Acer pseudoplatanus L. in the Kew reference microscope slide collection is discussed in relation to generalised statements in the literature on root wood anatomy.

Description: The variation in wood anatomy within 30 hardwood species, each with a distribution covering both rain forest and savanna areas of the Ivory Coast, Africa, has been studied. Compared to specimens from the rain forest, material from the savanna tends to have more wood ray tissue (rays are higher, wider, and more numerous) and slightly more vessel tissue (vessels are more numerous and wider, although they are often composed of shorter vessel members). Within any one species the total amount of axial wood parenchyma in the material from both areas is practically constant. The results are discussed with reference to latitudinal variation and major trends of phylogenetic wood specialization.

Description: A theoretical flow model shortly to be published elsewhere describes the rate of axial flow of liquids, through conifer wood in response to known pressure differentials. This is based on certain assumptions as to the structure and ultrastructure of wood. The model predicts very different flow conditions for earlywood and latewood cells. While these predicted conditions are approximately similar to those observed experimentally by tree physiologists, it is not yet clear what advantages the reduced conductivity of latewood cells could convey to the tree.

Description: The shedding of branches along a preformed layer is a complex phenomenon in which several types of xylem elements are involved. The abscission layers in Perebea mollis and Naucleopsis guianensis are distinguished from the normally developed xylem by the presence of shorter unlignified fibres with small simple pits. Most of these fibres show large nuclei. In this zone containing abnormal fibres, the vessels, rays and parenchyma are conspicuously different from those of the normal tissue. The transition in anatomy from the main branch to the abscission layer is much more abrupt than that from the abscission layer to the secondary branch. Contrary to what is generally seen in other Moraceous tribes, natural pruning seems to occur in all genera of Olmedieae with the sole exception of the genus Olmedia. The correlation with other morphological and anatomical characters and the complexity of the phenomenon of branch abscission seem to justify Berg’s decision to use this character in defining the new tribe Castilleae, containing all the genera formerly placed in Olmedieae except Olmedia.

Description: The author supposes that the fossil content of thin carbonate units in the Upper La Vid shales (Lower Devonian) of Colle was influenced by heavy storms like hurricanes. Apart from microplankton (Cramer, 1964) no fossils are found in the shales. Together with the very well developed fissility of the shales this points to abiotic conditions, probably caused by the lack of oxygen in the deposition area. Alterations, e.g. by storms, of the water circulation pattern in the basin destroyed this situation, and a pioneer fauna was able to develop. Sometimes storm debris, probably deposited by hurricanes, served as a substrate for larvae which settled in the area. Little by little the former situation of lack of oxygen returned and the communities died.

Description: In the delta of the rivers Fluvia and Muga, the Quaternary is hydrogeologically the most important deposit. It is underlain by Pliocene marls and clays. From geo-electrical soundings and bore-hole data a map with depth contours of the Quaternary-Pliocene boundary plane was constructed. Near the coast the Quaternary consists of two aquifers. One of the restrictions of the resistivity method is that the second aquifer is too thin in respect to its depth. Therefore only the formation resistivities of the complete Quaternary were calculated. By comparing the map of formation resistivities with maps of the clay percentage and the water resistivities in the Quaternary, prospective areas for waterwinning can be delineated. To the north of the delta, Silurian granites and schists crop out. A gravimetric survey over the contact shows a gently sloping boundary of the granite and schist with the Eocene-Pliocene of ca. 15°. From geo-electrical data a comparable inclination of 10° was found. The pre-Eocene topography here is thought to have been formed under tectonic control but the inclination of the Eocene-Pliocene to granite/schist would seem to be too shallow to correspond to a normal fault plane.

Description: Otoliths of 10 new species, including nine Gadidae from different localities in the North Sea Basin (Middle Oligocene — Upper Pliocene) are described: Gadus parallelus, Trisopterus concavus, T. incognitus, Colliolus parvus, C. johannettae, C. schwarzhansi, Palaeoraniceps regularis, Molva primaeva, Brosme heinrichi and ? Macruridarum deurnensis. Three new genera are established: Protocolliolus, Neocolliolus and Palaeoraniceps. Type material of some fossil otoliths of Gadidae described by Koken (1884, 1891) has been studied; as a result some systematic errors are corrected. The existence of two recent species of coal-fishes (Pollachius virens (L.) and Pollachius carbonarius (L.)) is ascertained by study of their otoliths.

Description: To explain the typical form of the anuran body, the following hypothesis is proposed: The ancestors of Anura, Urodela and Gymnophiona, having probably much in common, were potential competitors, so they each had to develop in a different ecological direction: Gymnophiona in the soil, Urodela on the surface of the soil specializing in the capture of slow moving prey and the Anura on the surface of the soil in the hunting of swift moving prey. Presumably the ancestors of the anurans were slow animals themselves and had to wait hiding until prey passed by. Also, to protect the body against dehydration it was necessary to dig into the soil and — because of the need to catch swift moving prey — to dig backwards, so that the head remained free. In the following discussion several characteristics of recent anurans and of probable ancestral anurans are examined in the light of this hypothesis.

Description: Five halacarid species, found in the mesopsammal of Caribbean Islands, are described, viz. Halacarellus tropicalis n. sp., Copidognathus grandiosus n. sp., Agaue arubaensis n. sp., Scaptognathus ornatus n. sp., and Limnohalacarus cultellatus Viets, 1940. H. tropicalis is the first member of the genus Halacarellus reported from tropical beaches.

Description: Seven springs in the Middle Atlas and five in the Rif have been studied. These show a great diversity of crenal habitats: water temperature ranges from 8.7° to 21°C, and the flow from 1 l/s to 1,800 l/s. Based on hydrologic and thermic characteristics, a spring typology is provided. The invertebrate community consists of 60 species, among which 4, found in the Rif, are new to science: Protonemura sp. (Plecoptera), Obuchovia sp. (Diptera, Simuliidae), Rhyacophila fonticola n. sp., and Philopotamus ketama n. sp. (Trichoptera). The new Trichoptera are both described. Two rare endemic species (the planarian Acromyadenium maroccanum and the coleopteran Elmis atlantis) have been found in a cold-water spring in the Middle Atlas; two black-fly species ( Cnetha carthusiensis and Simulium lamachei), new to North Africa, have been collected in a cold-water spring in the Rif. The cold-water spring community shows a high rate of endemism. Seven endemic cold-stenothermous species constitute a most characteristic crenon fauna in northern Morocco. The fauna of warmer springs (18° ≤ temp. ≤ 21°C) contains potamophilous and thermophilous species, a few of them belonging to the Ethiopian fauna. A comparative study of spring and rhithric communities of Morocco shows that, in the Middle Atlas and the Rif, cold-water springs became refugia for cold-stenothermous, west-palaearctic species; in the past, these species occupied a larger territory which has been reduced after recent climatic and hydrologic changes.

Description: Rates of food uptake were measured for individually reared larvae of the spider crab Hyas araneus L. feeding on freshly hatched Artemia nauplii at constant 12 degree C. Feeding rates (FR) of crab larvae were given as number of nauplii and amounts of dry weight, carbon, nitrogen, hydrogen, and energy (estimated from C) consumed per day. In both zoeal stages FR increased during postmoult and intermoult, remained high during early and intermediate premoult, and decreased again during late premoult. No clear pattern was found in the course of daily FR of the megalopa. Gross growth efficiencies (K sub(1)) showed a dramatic decrease from postmoult to early premoult (〉 60 to 〈 20%) in both zoeal stages. Daily consumption expressed as % body weight also decreased significantly in these instars. Average daily FR were highest in the zoea II, lowest in the megalopa, and intermediate in the zoea I. Since development of the megalopa took the longest time, the total amount of food consumed by this instar was equal to consumption in both zoeal stages combined.

Description: Duration of development in the larval and early juvenile stages H. coarctatus was studied in relation to temperature, and compared at extreme (18 and 6 °C) than at intermediate (9 to 15 °C) temperatures. The results were used to estimate the duration of development from hatching to the third crab stage in the field. Settling and metamorphosis was predicted to occur mainly during June. Biomass increased exponentially during larval development. Juvenile growth was also exponential and was maximum at 9 degree C, and minimum at 18 and 6 °C.

Description: Statistically significant differences were found in development duration of Hyas araneus L. larvae hatching on different days from the same egg batch. Larvae from different females show a decreasing trend in development time the later they hatch during the season. This trend was found in all larval instars; it was particularly apparent in the megalopa. Development durations in the 2 zoeal stages are positively correlated with each other, i.e. individuals developing slower than the average in the first larval instar tend to delay moulting also in the second instar. There are negative correlations between larval development time in all stages and the size of juvenile crabs, i.e. weak individuals tend to develop more slowly and to become smaller juveniles than the average. These larvae show lower accumulation rates of biomass already during the first zoeal stage. Larval development rates (at 12 °C) were not clearly affected by the temperature prevailing during previous embryonic development, but embryos incubated at higher temperatures tended to become smaller crabs.

Description: Exuvial losses in relation to late premoult matter and energy, and in relation to growth achieved during each instar, were studied in laboratory-reared larvae and early juveniles of the decapod H. araneus (L.). Changes of composition during development were measured in the complete body and in the exuvia from hatching through the second crab stage. Rates of exuvial loss increased during development in all parameters measured. They were generally highest in inorganic carbon and lowest in N. six to 7% of late premolte energy was lost by moulting zoeae, i.e. 9 to 13% of the energy produced during these stages. The megalopa lost 13%, and juveniles 19 to 20% of their LPRM energy ( similar to 29 to 41% of growth). During complete larval development of H. araneus a total of 18% of produced energy was lost at ecdysis. The same amount had been reported in the literature for larval development of 3 other decapod species.

Description: The influence of continuous and differential transitory starvation on the moult cycle and morphogenesis of H. araneus L. larvae was studied in laboratory experiments. Larvae starved from hatching (zoea I) or from moulting to later instars (zoea II, megalopa) develop, independently of food supply, to Stage C (intermoult). Postmoult Stages (A and B) and parts of intermoult are completed by utilizing internal body reserves under such conditions but cuticle formation is terminated at an advanced but incomplete stage within intermoult. In the zoea-II instar there is morphogenesis in appendages (pereiopod and pleopod buds) during continuous starvation. This supports the hypothesis that moult cycle and morphogenesis may be partly independent processes which are normally synchronized.

Description: (1) D. rathkei exhibits negative phototaxis during the whole day. It never leaves the sediment as long as there is any light. (2) The vertical migrations into the pelagic environment, as observed in Aug and Oct, start ca.1 h after sunset; they have their maximum intensity from ca. 22.00 h to 23.00 h and end at midnight. D.rathkei reacts positively to light during this time. (3) Fish and other predatory animals are almost inactive during this period. Population loss by predation is thus negligible or even lacking. (4) The literature on the 'hyperbenthos' is critically discussed in relation to the method mostly employed, the use of Beyer's epibenthic closing net. This gear is not considered to be useful, and the results obtained by it are doubted. (5) D. rathkei has no significance at all for the 'hyperbenthos'. The existence of this community in the Western Baltic Sea is doubted.

Description: The annual cycle and distribution of the benthic copepod fauna of a shallow inshore area in the south of podfauna of a shallow inshore area in the south of Kiel Bay (Baltic Sea) were investigated. The spp composition found is not typical for medium fine sand, but resembles that characteristic of a mixture of coarser sand, phytal and even soft bottoms. The mean population density was ca. 10 times smaller than in off shore stations. Obvious maxima were observed in July and Nov, and attributable to different spp. The dominant harpacticoid spp change several times during the year. Spp diversity was highest in summer, lowest in winter, when only 2 spp, Paraleptastacus holsaticus and Scottopsyllus minor, were dominant. Many spp show breeding maxima in spring and summer, a few in autumn (e.g. Ameira parvula) or winter (e.g. Scottopsyllus minor). The effect of sewage pollution manifests itself significantly only in the immediate vicinity of the outfall: spp diversity decrease; Scottopsyllus minor, Nitocra spec., N. tuypica, Paraleptastacus holsaticus, Parastenhelia spinosa, as well as Tachidius disciples are rather frequent in this zone. The potential value oft hese spp as indicators of water quality is discussed. Most of the harpacticoids in the investigated area are rather tolerant to domestic waste products.