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: The water economy, the mineral content of the soil, and human influence are the principal ecological factors governing the variation of the heath vegetation of a limited region. Sloping of the surface is also an important factor. In hilly country it is of a twofold nature: on the one hand the difference between high and low altitudes, based on the water economy, on the other hand differences in (micro-) climate. If the hills are higher, this results in greater climatic differences. In extremely oceanic and in boreal regions a rise in altitude of 100 m is sufficient for creating a noticeable decrease in temperature and an increase in precipitation, aerial moisture, and wind force. This results in the occurrence on the hills of heath communities that have their main distribution more to the North. The same observation was made by Gimingham (1961). On Slieve League on the Donegal coast (Ireland) Salix herbacea and Lycopodium selago occur in the heath at an altitude of 600 m, near Tongue on the Scottish north coast Dryas octopetala, Saxifraga oppositifolia, Alchemilla alpina and Thalictrum alpinum at an altitude of 60 m. West of Apeldoorn in the Netherlands are found extensive stretches of heath with abundant Vaccinium myrtillus and V. vitis-idaea at an elevation of 60-80 m, even on south-facing slopes. This is an area with high precipitation due to ascending air west of the hill ridge of the Eastern-Veluwe. Here the Vacciniums, elsewhere requiring the protection of the forest, can tolerate the habitat of the open heath (Stoutjesdijk, 1959; De Smidt, 1966). Higher elevation combined with north-facing slopes creates extreme conditions e.g. on Roc Trévézel (300—360 m) in Brittany, with Vaccinium myrtillus, Melampyrum pratense, Hymenophyllum wilsonii and Rhytidiadelphus loreus. These species are virtually lacking in the surrounding plains where the heath consists of such South Atlantic species as Erica cinerea, E. ciliaris, Ulex gallii, Lobelia urens, Lithospermum prostratum and Symethis planifolia.

Description: From the general discussion of the effect of mass selection on the genotypic array of the next generation we have seen that under certain conditions mass selection can lead to homozygosity, but does not do so necessarily. Outcrossing, mutations and disadvantages of certain genotypes may prevent reaching equilibrium condition with complete homozygosity even in the simplest case of one locus with two alleles. It depends on the magnitude of these factors and the degree of heterozygosity of the variety how close to genetic uniformity we ultimately can come. The advancing of one generation has only a small effect, which becomes less as the frequency of one of the genotypes becomes less. Mass selection can reduce segregation in a variety, but only in ideal situations and only in small steps. Obviously the most effective way to promote genetic uniformity is to begin with non-segregating material obtained through careful inbreeding and within-family selection. Then, if this is available, mass selection is hardly necessary and seed collection should be done so as to prevent a return to a heterozygous condition. When only segregating populations are available, some changes can be expected if the selection intensity is low, but they will not be great and may not be noticed until after several generations. Returning to the original question of the stability of the tobacco variety, the conclusion can be drawn that when large numbers of plants from a field are selected as seedplants the changes in the next generation as a whole will be small, regardless of the selection procedure used. When 10-30 % of all plants are allowed to produce seed we cannot expect important changes. Also, when the environmental variations are as great as in shade tobacco, the possibilities of selecting against certain genotypes for a number of characteristics simultaneously becomes virtually impossible. Concerning whether or not mass selection can lead to improvements in the variety, it was explained that the selection intensity and the heritability of a character determine the selection response. Perhaps this response can be predicted in the case of one character, but it becomes difficult, if not impossible, to forecast the results when many characters are involved at the same time. Reference was also made to a selection index which has been effective in livestock breeding. Even if an index could be determined for shade tobacco, its use is not necessarily effective, as Kempthorne (1957) pointed out. The genotype-environment interaction makes questionable the choice of certain fields over others. Without experiments, such questions cannot be answered. It is likely that mass selection with low selection pressure changes a variety very little. Again, in a field where up to 30 % of the plants are selected for seed, the pressure cannot be very great and we should not expect great changes. Only when a few plants are carefully selected for certain characters should progress become noticeable, as is the experience of single plant selection in plant breeding. We conclude that mass selection for seed and plant breeding to improve a variety should not be confused with each other. Each has its own aims and methods, which are not interchangeable. Where uncertainty exists about seed, progeny tests usually are made to compare a seed with the parent seed. Bolsunov (1959) has described a number of such procedures for tobacco, though the more elaborate of them appear impractical.

Description: A survey is given of the types of the sclereids and the sclereid patterns occurring in the leaves of the Marcgraviaceae. Eight main categories of sclereids are distinguished on the base of the morphology of the sclereids. A comparison is made with the foliar sclereids found in some other families. The systematic value and the function of the sclereids are briefly discussed. Some new combinations of names are published.

Description: Eight species of the genus Sanguisorba L. were studied. Two distinct types could be recognized, viz., the Sanguisorba minor and the Sanguisorba officinalis type. Sanguisorba filiformis (Hooker fil.) Handell-Mazzetti appeared to be a transition between these two types.

Description: The pollen assemblages of a core in the coniferhardwood formation in northwestern Minnesota are compared with the floristics of the recent vegetation in the region. Percentage levels of the main tree components have been compared first with those from recent surface samples taken at the same short distance from various types of upland forests and second with the regional values of the pollen rain in this area (McAndrews 1966). To that end all the data were recalculated on the basis of special pollen sums. The regional diagram of Stevens Pond shows basically the same assemblage zones as established by McAndrews but without the late-glacial Picea-Populus assemblage zone. The pollen in the following Pinus-Pteridium assemblage zone has been interpreted as derived from a pine forest. During the midpostglacial expansion of the prairie eastwards the regional vegetation must have been a Quercus savanna, locally with prairie. Corylus reaches relatively high percentages in this zone. Among the prairie elements especially the occurrence of Lilium philadelphicum may be noted. In the next zone the pollen diagram shows a rise of the curves of mesic elements. In spite of this the comparison with recent surface samples indicates a xerophytic Quercus forest rather than a mesophytic deciduous forest. In the following Pinus assemblage zone pine was present along the margin of Stevens Pond and is therefore overrepresented in the diagram. In the uppermost zone the pollen curves show the effect of logging of the forest about 1900. Pollen of cultivated and introduced plants appear in this zone. Many local pollen types were found, on account of local overrepresentation. This made it possible to compare the local Stevens Pond sequence with the composition of recent lowland vegetation types. The pollen sequence was similar to a large extent to the recent pattern of lake filling, starting with a eutrophic vegetation of Typha latifolia and Salix in the prairie period and leading to a Larix forest and then to a mesotrophic Picea mariana forest, the present edaphic climax on peaty soils. There is a delay, however, in the introduction of acidophilous species, the Larix forest being without Sphagnum and Ericaceae. This is explained by assuming an influence of the vegetation of the surrounding slopes upon the local vegetation. About 1900 the bog forest was destroyed by logging operations and replaced by the present Typha latifolia mat.

Description: Arbor 8 m alta, altitudine pectoris 20 cm diam.; ramuli teretes, glabri. Folia coriacea, glabra, plana, late elliptica vel late obovata, apice obtusa, rotundata vel subacuminata, basi attenuata et in petiolum decurrentia, 9-12 cm longa, 5-7½ cm lata, statu sicco supra viridia, leviter nitida, infra olivacea, opaca, marginibus subrevolutis, integris; costa et nervi primarii utraque facie prominentes, nervi primarii infimi tenues, inconspicui, spatio brevi margine paralleli, ii paris secundi costae paralleli et valde proximi supra basin folii, tum divergentes sub angulo 30°, plus minusve recti inter costam et marginem et 1-1½ cm a margine remoti, nervis primariis paris tertii coniuncta in parte tertia superiore laminae; nervi primarii tenuiores singuli vel plures primariis maioribus intercalati; venae secundariae leves, paucae, ad marginem et apicem laminae arcuatim coniunctae, rete supra occulto, infra minime claro; petiolus 1-2 cm longus, 2 mm crassus. Inflorescentiae axillares, 10-14 cm longae; rhachis glabra; flores geminati; pedicellus communis perbrevis, pedicellus communis cum individuali 4-4½ mm longus, glaber; bracteae minimae, triangulares mox deciduae; alabastra cylindrica, apice clavata, lutea, 8-9 mm longa; lobi perianthii glabri, crassi, apice leviter excavati, 8-9 mm longi, 1 mm lati, anthesi recurvati, pallide flavo virides; filamenta brevissima, lata, parte superiore loborum perianthii affixa; antherae 2.6 mm longae; ovarium brevissime et adpresse fusco-pilosum, 2 mm altum, sensim in stylum protractum; stylus apice leviter clavatus, stigmate terminali; glandulae disci quaternae liberae, crassae, subglobosae, 0.4 mm altae et latae. Fructus ignotus.

Description: Some of the basic concepts common to plant taxonomy, palaeobotany and palynology are discussed such as “taxon”, “taxonomic categories”, “genus and species concepts”, as well as “organ and form genera”. The development of the specifically palaeobotanical and palynological concepts of organ and form genera is briefly treated in the light of the shaping of palaeobotanical thought and methods since Adolphe Brongniart. The need for a single category of an artificial nature (i.e., form genus) is acknowledged; the need for a second category of such nature (i.e., organ genus) is questioned. The general guide lines for good palynological practice given by Faegri et al. (1950) are recommended for future use and are reprinted as an appendix to this paper.

Description: Index to the Enumeration of the Orchidaceae of Sumatra, by J.J. Smith. At the Rijksherbarium there was a handwritten copy compiled by the late Dr. J.J. Smith of his important enumeration of Sumatran Orchids, published in Fedde, Repertorium 32 (1933) 130-386, which was obviously for reasons of economy not printed. The author left a note to the Librarian of the Rijksherbarium saying that it is indispensable for consulting this work, as many orchid names were here reduced to synonymy for the first time. This is now available for orchidologists and libraries in stencilled form in the same format as the Enumeration, with the Library of the Rijksherbarium, Schelpenkade 6, Leyden, Holland.

Description: Field work on the Ceylon Flora. Trimen’s ”Handbook” on the flora of Ceylon, published between 1893-1900, is one of the finest floras ever written of a tropical area. It is a five volume descriptive work that served very adequately for many years. It is now not only out-of-date, but completely unobtainable. The Smithsonian Institution, in cooperation with the University of Ceylon and the Royal Botanic Gardens, Peradeniya, is initiating a project to bring up to date and republish the Trimen ”Handbook” by providing an opportunity for field work in Ceylon.

Description: *Allen, B. Molesworth: Malayan Fruits. An introduction to the cultivated species (with Thai and Tamil names). 1967, 245 pp., 73 fig., 10 photo., 1 tab. 8°. Donald Moore Press Ltd. Singapore. M$ 7.50. A popular guide in a handy well illustrated and wellprinted cheap hook of the most common edible fruits. By the ”quick guide” on the table one can orient himself on the identity; also within the genera there is a key to the species or varieties. Each species is fully described and for the layman a glossary of botanic terms is added, for the housewife a list of recipes.

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: The practice of citing collections made in institutional series by the letters of that series instead of by the collector’s name (e.g. FB 23435 instead of Aquilar & Valderrama FB 23435) led, with the publication of so many Identification Lists, to the dishing out of an alphabet soup that many a botanist or curator of collections may find hard to digest. In itself, the system of collecting in long institutional series is an excellent one, permitting great economy in space when collections are to be cited. The oldest series seems to be the KB-one, dating from about 1870, established by Scheffer, followed early in this century by the BS and FB series, established by Merrill. A good number-stamp may have contributed much to the success and consistency with which the series were maintained for a long time. In other institutes, there has been created what Dr. Ashton characterized as ”a masterpiece of confusion”, the unravelling of which, as can be seen from his paper on ”The numbering of Sarawak Forest Department collections” in this Bulleton on pp. 1432-1435 (1966), requires a good deal of research. The purpose of this paper is only to give a list of abbreviations in use between Thailand and the Solomons, for the guidance of those who compile, and those who use Identification lists. These Lists, products of the work for the Flora Malesiana, serve as documentation as well as being of use for the identification of Malesian duplicates not seen by a taxonomist himself. When compiling and using such a list, three questions are to be considered.

Description: Since the last Bulletin was published we have to regret the loss of one of the last of the Mohikans of the Treub period of ’s-Lands Plantentuin (Kebun Raya Indonesia) at Buitenzorg (Bogor), namely of Dr. Charles Bernard, born 1876 in Geneva, who died at Amsterdam, 29th July 1967, aged 90. He studied at Geneva, finished his education by getting his degree in 1894, after which he remained for six years assistant to Prof. Dr. R. Chodat under whom he prepared a doctor’s thesis in 1901 (published 1903) on the embryology of some parasitic plants which led him to consider Lathraea as a scrophulariaceous genus.

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: 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: My visit to and trips in Taiwan, in 1966, brought me into close contact with the wonderfully rich and varied flora of this large island which is fairly easily accessible if one speaks Chinese or is accompanied by Chinese companions, as was my privilege. As is well known the woody flora of Taiwan is tolerably well known, by the excellent work of Kanehira (1936), followed by the modern works of Prof. Tang-shui Liu (2 vols, 1960-1962) and Prof. Li (1963).

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: Einige zur Ascomycetenfamilie der Sporormiaceae gehörende, aus dem Erdboden isolierte Pilze werden als Arten der Gattungen Sporormia (Synonym: Sporormiopsis), Preussia (Synonym: Honoratia) und Westerdykella (Synonym: Pycnidiophora) besprochen und mit einander verglichen. Sporormia aemulans var. ostiolata wird neu beschrieben. Einige als Sporormia und Preussia beschriebene Arten werden mit Preussia fleischhakii vereinigt.

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: Five species of Ganoderma Karsten are discussed, which are confined to the tropics and characterized by the presence of a light-colored context, but which are devoid of the laccate upper surface of the pileus typical of the species of the Ganoderma lucidum-group. Ganoderma neurosporum J. Furtado is proposed as a new species. Three of the five species—Ganoderma amazonense Weir, G. coffeatum (Berk.) J. Furtado, comb, nov., and G. neurosporum J. Furtado—are from the neotropics. Ganoderma lloydii Pat. & Flar. is known only from Africa, and G. asperulatum (Murrill) Bres. has been reported only from the Philippines and Borneo. Regardless of their geographical distribution, the five species under discussion are distinguished particularly by their basidiospore characteristics. In their morphological features they show several characteristics also found in some trocial species of Amauroderma Murrill.

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: This paper complements the revision which before long will appear in the Flora Malesiana, where a key to all species will be given, and descriptions of the Malesian taxa over their whole area; the few non-Malesian taxa are here described. It accounts for the complete synonymy (147 binomials) and typification, with the literature relating to the regions adjacent to Malesia. An Identification List of all examined specimens was separately issued in the Flora Malesiana Lists, number 27 (1966) 430—442; the Herbaria which supplied the materials are: Arnold Arboretum (A), British Museum, Natural History (BM), Bogor (BO), Brisbane (BRI), Cambridge (CGE), Dehra Dun (DD), Gray Herbarium (GH), Kew (K), Leiden (L), Leningrad (LE), Michigan (MICH), Sydney (NSW), Paris (P), Manila (PNH), Singapore (SING), Utrecht (U), Berkeley (UC), and Washington (US). Thanks are due to the directors of all these institutions.

Description: A complete revision is given of the Indo-Malesian genus Cratoxylum. The subdivision of the genus into 3 sections, as given by Engler (1925) and Corner (1939), has been found correct. The characters by which these sections are discriminated concern the interpetiolar scars on the twig, the type of venation, the occurrence of petal-scales and their shape and size, the shape of the hypogynous scales alternating with the three staminal phalanges, and whether the seeds are surrounded by a wing or are winged on one side only. Each section contains two species. A concise review has been given about the history of the genus, an account of the uses made of it, and the ecology. It appears that almost all species can act as pioneers for which they are fully qualified by their euredaphic requirements and early and abundant seed production. Though some species, notably C. arborescens and C. glaucum, are evergreen, and C. formosum is deciduous, the others are not specifically one or the other way round; in C. maingayi Corner noted that sometimes particular branches shed their leaf. There is no major correlation between leaf-shedding species and seasonal climate regime. A brief summary is given on the morphology, in particular the structure of the inflorescence. Two points have not become entirely clarified, for example, whether all species are always heterodistylous: this should be studied further in the field. Another point is the want of more exact data on the degree in which the ovary is incompletely celled which seems to differ from one species to another, and to compare this with the ovary of the allied Madagascan genus Eliaea (vide infra). C. glaucum excepted all species show a distinct variability. In three species this is grading and no infraspecific taxa can be distinguished in a key on the basis of herbarium material. Within Malesia the variability is more or less of a geographical character and could be classified under clinal variation. This is also the case in C. sumatranum and C. formosum, within which I can distinguish, however, three and two infraspecific taxa respectively, which accordingly have been given racial rank, that is, as subspecies. Within each a still finer distinction might be feasible of subsubraces which mostly coincide with separate islands of Malesia. The closest related genus is the monospecific genus Eliaea Camb. from Madagascar with which it forms a tribe of the Guttiferae. With regard to the exact structure of the ovary claimed to be distinct from that of Cratoxylum a close comparative-morphological study should be made of the ontogeny of the ovary in Eliaea and all species of Cratoxylum. Except from taxa described by Loureiro, Jack, and Blanco, of whose names no types seem to exist, I have for the first time examined type material of all names and checked their detail floral characters which were often not mentioned in the original diagnoses. A listed account of all numbered material on which this study was based will be published in a separate ‘Identification List’.

Description: The populations of the seaward intertidal ends of the 1955 lava flows in Hawaii were studied during the first few years of their development. Different seral phenomena were recognized such as pioneer colonization, succession, disclimax, and subclimax. The term climax is used as a practical term to denote existence of an equilibrium between the populations and the environment. Appearance of the climax situation seems to be related to stability of the substratum for a period at least as long as six to ten years, but even populations on surfaces as old as 100 years are different from some that are on adjacent prehistoric surfaces.

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: This study considers the 163 species accepted as belonging to the tribe Arundinelleae (Gramineae) and arranges them into a putative cladogram. A discussion of the rationale is presented, 38 characters are studied for advanced versus primitive states, advancement indices calculated, and trends of variation discussed. The six major groups of Phipps (1966b) are maintained. The phylogeny conforms excellently with the geographical aspects of the continental drift hypothesis though it requires a greater age for the Angiosperms than is generally held to be the case.

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: New details could be derived from the study of fixed male and female flowers of Scyphostegia borneensis Stapf. Of prime importance among these is the exact structure of the female reproductive units. They correspond to what are generally recognized as ovules. These anatropous ovules have a constriction separating funicle and raphe, an aril (loid) of mixed character, a distal integumental extension, and a fivelobed exostome. Their placentation is basal. Together, they are enclosed by an urceolate wall consisting of three-trace units which are apically stigmatic. These sterile units form septs growing downwards between the tips of the ovules, giving rise to locules which are open below. The morphological interest of some of these details was discussed. The embryosack development could be followed. The fruit appeared to be a fleshy capsule. The striking similarity with certain formations in the Monimiaceae is not based on affinity. As to the above characters the alleged affinity with the Flacourtiaceae could not be checked because comparable characters in that family have never been studied. However, there is a correspondence with such details known in the Tamaricaceae. Moreover, in the Tamaricaceae the placentation is intermediate between basal and parietal. This was considered to favour the inclusion of the Scyphostegiaceae in the Parietales. Of all the Parietales families they must be nearest to the Flacourtiaceae, as judged from external characters.

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

Description: In a recent survey of algal taxonomy published for the use of Danish university students, the author (1962, 1966) has introduced some new taxa and names. A few of them express new systematic opinions, and will be separately accounted for. The majority have been made for formal reasons only, and are established here in accordance with the code of nomenclature.

Description: In a recent paper by Mrs. Gray [J. Arnold Arb. 43 (1962) 74] a new species of Podocarpus was proposed from Morotai, P. filicifolius. Inasmuch as the description of the leaves corresponds exactly with juvenile P. vitiensis (not previously reported from the Moluccas) and the description of the fruit corresponds exactly with P. blumei (whose range includes the Moluccas), it was of interest to confirm whether the fruit in question was attached to the foliage material described. An examination of the specimen ( Kostermans 1949), in Leyden revealed that the fruit was collected separately and that sterile specimens of P. blumei were also collected in the general vicinity ( Kostermans 1660, 50 m). Dr. van Steenis kindly wrote to Dr. Kostermans concerning the particulars of the collection of these specimens. Kostermans writes: ‘Kostermans 1215 of G. Pare-Pare, 1000 m (apparently the same as the unnumbered specimen in Leiden), I picked from a sterile treelet c. 3 m high. There is an unidentified specimen of it in Herb. Bog., which looks to me like P. vitiensis.’ ‘Kostermans 1660 is also sterile. I remember to have cut a large tree in Morotai which fell into a ravine after cutting and remained out of reach; that was a Podocarpus and presumably we have picked some fruits from the ground.’ ‘I quite well remember the collecting of P. vitiensis on top of G. Pare-Pare; almost all of it (?) was sterile, but still I found it necessary to collect samples. P. neriifolius was certainly on this ridge, but no P. blumei.

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: In the course of a revision of the Malesian genera included by Radlkofer (Pfl. Reich Heft 98, 1932) in the Sapindaceae-Aphanieae and Lepisantheae, attention had to be paid to the genus Phoenicimon Ridl. Ridley described it in the Sapindaceae and expressed its supposed relationships more precisely by giving it the number 7A, between 7 Lepisanthes and 8 Otophora, and by adding the note ‘Apparently most nearly allied to Otophora .... ’ A study of both syntypes of Phoenicimon rubiginosus Ridl., the only species, and of some more specimens revealed its true identity as a species of Glycosmis in the Rutaceae. This identification was confirmed by Dr. C. G. G. J. van Steenis and by Dr. R. C. Bakhuizen van den Brink.

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: 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: Dr. McClure’s studies on the bamboos date from a period of service in China, at first as an Agricultural Explorer, since 1931 as a Professor of Botany at Lingnan University in Canton. On field trips in the Chinese interior and in Indo-China he collected numerous living bamboos, which were transplanted and studied in the to-day still intact Lingnan Bamboo Garden he had early established. After in 1941 the war had forced him to leave China, he studied living bamboos in the West Indies, Central and South America, and after the war in India, East Pakistan, Java, and Luzon. Being particularly interested not only in morphology, but also in taxonomy, he revised the bamboo collections of several herbaria in the United States and Europe. Proof of his comprehensive knowledge thus acquired is given in his book, which indeed brings the economically important and scientifically interesting, but for various reasons much neglected bamboos into fresh perspective. Students both in pure and applied botany will find here a wealth of information, based on the author’s personal experience as well as on his familiarity with the pertinent literature.

Description: A description is given of the arrangement cf the mafic and ultramafic rocks within the metamorphic complex in Galicia (NW Spain), followed by a brief petrographic description of some frequently found metamorphic types. Differences in metamorphic state and field relations lead to the conclusion, that mafic rocks have been emplaced in this complex in at least three distinct periods and that the two later phases are perhaps due to a process of remobilisation of mafic metamorphic rocks.

Description: Several recent papers have described ecological differences between sympatric species of Anolis in the Greater Antilles (RUIBAL 1961, COLLETTE 1961, RAND 1962, 1964, 1966). A three day visit to Curaçao in September, 1962, provided an opportunity to make field observations on a species of Anolis that occurs with no congeners. These observations suggest that it occupies a microhabitat somewhat broader than most of the Antillean species. This trip was undertaken with the financial support of National Science Foundation Grant No. 16066. Specimens collected were deposited in the Museum of Comparative Zoology, Harvard University.

Description: The Lesser Antilles consist of those West Indian islands which extend from the Anegada Passage in the north to Grenada in the south.¹) These islands are nomenclatorially divided into two major groups: 1) The Leeward Islands, including Sombrero, Anguilla, St. Martin, St.-Barthélemy [= St. Barts], Saba, St. Eustatius, St. Christopher [= St. Kitts], Nevis, Redonda, Montserrat, Barbuda, and Antigua, and 2) the Windward Islands, including Guadeloupe (with its satellites Marie-Galante, La Désirade, Les Saintes), Dominica, Martinique, St. Lucia, St. Vincent, Grenada, and Barbados. Geologically, the Lesser Antilles can be divided into two major groups: 1) those which are mountainous – the so-called inner-chain islands – which are younger and more recently volcanic (Saba to Grenada, and including the western or Basse-Terre portion of Guadeloupe, and Les Saintes), and 2) the older, gently rolling limestone islands – the so-called outer-chain islands (Sombrero to Marie-Galante, and including the Grande-Terre portion of Guadeloupe, La Desirade, and Barbados). The northern Leeward Islands may be additionally grouped according to the banks on which they lie: the Anguilla Bank (incl. Anguilla, St. Martin and St.-Barthélemy), the St. Christopher Bank (incl. St. Eustatius, St. Kitts and Nevis), and the Antigua Bank (incl. Antigua and Barbuda). The Lesser Antilles extend for about 750 kilometers in a northwest to southeast direction on a slightly bowed arc. The mountainous inner-chain islands are generally very mesic, with the windward (eastern) coast wet and the leeward (western) coast dry; the latter lies in the rain shadow of the central mountains. This brief ecological statement is greatly oversimplified, since on some islands there are dry sections on the windward side (the Presqu‘île de la Caravelle on Martinique is a notable example) and occasional sections of the leeward coast are better watered than is customary (the central western coast of Dominica and the western coast of Montserrat are examples). The central mountains vary in maximum elevation from 1975 feet (602 m) in St. Eustatius to 4813 feet (1456 m) in Guadeloupe; Guadeloupe, Dominica, and Martinique, in that order, have the three highest peaks in the Lesser Antilles.

Description: After our studies about the marine mollusks of St. Martin, (COOMANS 1963a, 1963b), this publication will deal with the land and freshwater shells of the island. The non-marine mollusks of St. Martin were already fairly well known at the end of the last century (MAZÉ 1890, p. 22—34), who mentioned 36 species, mainly collected by H. E. VAN RIJGERSMA. VERNHOUT (1914) compiled from the literature the land and freshwater mollusks of the Netherlands Antilles, and he listed 37 species from St. Martin (not including 12 brackish water species). VERNHOUT’S list was entirely copied by SCHEPMAN (1915). Many specific names have changed since 1914, and more collecting was done on St. Martin during the last decades. This publication will cover all the species of non-marine mollusks known to us from the literature, from museum collections, and from our own collecting on St. Martin. One new subspecies of Adamsiella crenulata is described and figured here.

Description: The runoff in the Valle de Arán, which is a steep and high mountain basin in the Pyrenees, consists essentially of baseflow, and fast runoff is only a minor phenomenon. The baseflow is related to areas of scree and forest, and the percentage of the precipitation which contributes to the fast runoff, is related to the area of barren rocks. The orographic precipitation pattern has been statistically determined for eight valleys. It was found, that orographic precipitation increases linearly with altitude, while the maximum increase occurs perpendicular to the slopes of the steep mountain ranges. The expected errors, due to measurements of rainfall at 1.50 m above ground level, showed as a 10—15 percent error in the water balance. The Penman evaporation values were corrected for snow evaporation and they subsequently gave reliable results.

Description: In the present study the primary fluorescence phenomena of fossil pollen and spores are described. This new method in palynology is based on a large number of fluorescence microscopical observations and spectrophotometrical determinations of palynomorphs from deposits of various type and age. It resulted in three principles: the relationship between fluorescence colour to type or form of pollen and spores (Plate I and figs. 21—22), the change in their fluorescence colour from blue or green to red or brown with increasing geological age (Plate II, III and fig. 24) and a similar colour change with increasing rank of coal of the embedding deposits (fig. 33). These phenomena appear to be in accordance with other fossilization and coalification studies of fossil palynomorphs by various authors. For the preparation of pollen samples and the microscopical determination of fluorescence colours some special techniques have been adapted or developed. The discoveries of fluorescence palynology can be applied to various questions, as, for instance, the study of pollen morphology and corrosion susceptibility and the age determination of those deposits, for which conventional pollen analysis fails. Such datings of Cenozoic rocks can be carried out with an accuracy of more than 80 %. As an example a number of age determinations of contaminated sediments is given (Plate V). Besides, fluorescence palynology may be used to determine the rank of coal of palynomorphs in coalified rocks in that part of the coalification series, ranging up to a fixed carbon content of about 70 %. The explanation of the fluorescence phenomena described, meets still great difficulties, due to the inadequate knowledge of the chemical nature of the walls of fossil pollen and spores. Once again it is proved by this study that fossil palynomorphs are less resistant to fossilization and coalification than has been previously assumed.

Description: This excursion program anticipates the publication of a PhD. thesis (Vogel, in preparation) in this periodical and is intended as a guide to those points at Cabo Ortegal, that are readily accessible, well exposed and of general petrological interest. The described localities are indicated on a small map (fig. 1 ) and can also be found on the 1 : 25,000 topographical maps edited by the Cartografía Militar de España: sheet 1 (quadrants I, Cabo Ortegal; II, Ortigueira and III, Pontigás) and sheet 7 (quadrants I, Feria and IV, Cedeira) or on the 1 : 50,000 topographical maps edited by the Instituto Geográfico y Catastral, Madrid: sheets 1 (Ortigueira) and 7 (Cedeira). The author is grateful to Prof. Dr. E. den Tex for reading and correcting the text. EXCURSION I, duration 2 or 5 h.; to be made preferably on Sunday. Start before Bar Bahia, Cariño.

Description: 1. Se acuerda constituir el ”Grupo de Geólogos del N.W. de la Peninsula Ibérica” cuyo objetivo será facilitar e intensificar las investigaciones geológicas de la zona N.W. peninsular. 2. Los grupos fundadores son los siguientes: Dr. I. Parga-Pondal — Laboratorio Geológico de Lage. Prof. Dr. C. Teixeira — Museu e Laboratorio Geológico, Universidade de Lisboa. Prof. Dr. L. C. Garcia de Figuerola — Instituto Geológico de la Universidad de Oviedo. Prof. Dr. E. den Tex — Geologisch en Mineralogisch Instituut van de Rijksuniversiteit Leiden. Geol. Sr. R. Capdevila — Service de Geologie Générale, Université de Montpellier. Geol. Sr. Ph. Matte — Laboratoire de Geologie Structurale, Université de Montpellier. Geol. Sr. A. Ferragne — Laboratoire de Geologie, Université de Bordeaux. Geol. Sr. P. M. Anthonioz — Laboratoire de Geologie, Université de Poitiers. A los cuales podrán agregarse otros que se interesen por estos estudios.

Description: A short review of the literature on the stratigraphy of the Devonian and the Lower Carboniferous of the Cantabrian Mountains precedes the report of the author's stratigraphic and palaeontologic observations in León: the Río Esla area (Gedinnian to Viséan), the central Cantabrian area (Famennian to Viséan), and the Gildar-Montó area (Eifelian to Viséan); in Asturias: the coastal area (Frasnian to Viséan); in Palencia: the Arauz-Polentinos area (Gedinnian to Givetian), the Carda\u0148o-Triollo area (Eifelian to Viséan), and the San Martín-Valsurvio area (Givetian and Famennian to Viséan); and in Santander: the Liébana area (Eifelian to Viséan). Most of the conodont faunas, which were extracted from calcareous formations, could be arranged in the zonal succession established in Germany, and thus supplied new data about several formations in the Cantabrian Mountains. The presence of the transgressive Ermita Formation in Asturias and Palencia is demonstrated. The age of this unit ranges maximally from uppermost Famennian to lowermost Tournaisian. The Carda\u0148o Formation ranges from middle or upper Givetian to upper Frasnian. The Vidrieros Formation ranges from the upper part of the lower Famennian to the lowermost Tournaisian. A synthesis of the stratigraphic data delimits the Palentine facies area, which is clearly separated from the Asturo-Leonese facies area by positive areas. The following palaeogeographic units are distinguished: the Asturo-Leonese Basin, the Palentine Basin, and the Asturian Geanticline. The development of these units from the Middle Devonian to the Lower Carboniferous is demonstrated by eight facies-pattern maps. The sedimentation on the Asturian Geanticline was limited and probably incomplete. An epeirogenetic uplift of this geanticline took place in late Frasnian to early Famennian times. This uplift is correlated with the deposition of the quartzitic Murcia Formation in the sheltered Palentine Basin. The uplifted area was covered by the Ermita transgression in the late Famennian to early Tournaisian. After a break in the sedimentation, a local transgression resulted in the Vegamian Formation in the upper Tournaisian. In most of the area the Alba transgression began in the uppermost Tournaisian or lower Viséan. In the Palentine Basin the deposition of the Alba Formation started in the upper Viséan. The chapter on systematics deals mainly with the most important zonal guide forms of the conodonts. Three new elements are described: Icriodus eslaensis n.sp. from the middle to upper Givetian, Siphonodella? n.sp. a, probably from the upper Tournaisian, and n.gen. A n.sp. a, a simple compound conodont from the upper Gedinnian or lower Siegenian.

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.