A NEW STRUCTURALLY PRESERVED PENNSYLVANIAN CORDAITEAN POLLEN ORGAN

Permineralized specimens of the pollen organ Gothania (Hirmer) consist of a primary axis bearing pollen cones in the axils of bracts that are four ranked. The bilaterally symmetrical primary axis consists of a uniform parenchymatous pith surrounded by up to 15 endarch-mesarch axile bundles. The cortex is two-parted and consists of an inner zone of subepidermal fibers. Bract traces arise from the ends of the ellipsoid stele. Traces to the cones are derived from the open ends of the stele, and at higher levels form a centrarch-medullated vascular system. Each pollen cone is constructed of up to 25 helically arranged scales, each vascularized by a single trace that may dichotomize. Scales are elongate and broad, and histologically composed of mesophyll parenchyma and fibrous layers. Stomata are restricted to the adaxial surface between rows of fibers. Up to 10 distal scales may be fertile, each with 4 elongate pollen sacs at the tip. Large monosaccate grains of the Felixipollenites-type are densely packed in each pollen sac. The well-preserved specimens of Gothania provide an opportunity to compare this genus with pollen cones assigned to the genus Cordaianthus, and to relate isolated plant organs to the Cordaitales.     

STRUCTURALLY PRESERVED FOSSIL PLANTS FROM ANTARCTICA III. PERMIAN SEEDS

Small, anatomically preserved gymnospermous seeds are detailed from late Permian age silicified specimens collected in the Beardmore Glacier region of Antarctica. The seeds are platyspermic with prominent, sarcotestal wings and a simple pollen chamber. The integument consists of a narrow endotesta, a two-parted sclerotesta and a complex sarcotesta. In mature seeds, the nucellus is present as a papery layer, separated from the endotesta by a nucellar and endotestal cuticle. Cellular megagametophytes are present in many of the seeds and commonly contain two archegonia. A multicellular embryo is present within each archegonium. The embryos are at a similar stage of development and provide evidence of simple polyembryony in these seeds. Although the affinities of the seeds are not presently known, they are discussed in the context of other seeds described from Gondwana deposits, as well as the known flora from the Beardmore Glacier area.     

STRUCTURALLY PRESERVED PLANTS FROM SOUTHEASTERN KENTUCKY: STAUROPTERIS BISERIATA SP. NOV.

Several axes of the coenopterid fern Stauropteris are described from permineralized peat associated with Lower-Middle Pennsylvanian coal deposits of southeastern Kentucky. This represents the first documented report of the genus in North America. The specimens are regarded as representatives of a new species—S. biseriata—based on the distinctive branching habit. Three branch orders are described, and in each case, branches are singular and distichous, arranged in a two-ranked pattern. This is in contrast to other species of Stauropteris in which the branches are paired and form a quadriseriate pattern. A pair of vascularized aphlebiae subtend each branch through all branching orders. Aphlebiae associated with first- and second-order branches are three-parted at the point of insertion; those that subtend third-order branches are singular. Stauropteris and a number of Devonian fern-like plants are compared on the basis of certain morphological similarities.     

ON A NEW STRUCTURALLY PRESERVED ARBORESCENT LYCOPSID FRUCTIFICATION FROM THE LOWER PENNSYLVANIAN OF NORTH AMERICA

Bisporangiate lycopsid fructifications are described from petrifaction material of Pottsville (lower Pennsylvanian) age collected in eastern Kentucky. The largest specimen of Lepidostrobus schopfii sp. n. is 8.0 cm long and approximately 1.3 cm in diam; it is not complete at either apex or base. Basal megasporangia, each containing a variable number (12-29) of megaspores, and apical microsporangia are adaxially positioned on pedicels bearing reduced lateral laminae. Features of the cone axis and pattern of vascularization are described. Of particular interest is the occurrence of well-preserved endosporic megagametophytes showing archegonia and rhizoids. The new species is compared with other structurally preserved bisporangiate lycopsid fructifications of equivalent age.     

SPIRAL TUBULES IN PALM PHLOEM

Spiral tubule structures were observed in sieve elements of Pritchardia and Cocos palms. The spiral tubules were 80–120 nm wide and composed of alternating electron-lucent and electron-dense bands 11–16 nm wide which spiraled around a central core.     

STRUCTURALLY PRESERVED FOSSIL PLANTS FROM ANTARCTICA: II. A PERMIAN MOSS FROM THE TRANSANTARCTIC MOUNTAINS

An anatomically preserved moss from the late Permian of Antarctica is described. The fossils include delicate, unistratose leaves and axes with numerous rhizoids preserved in a silicified peat. Leaves exhibit a multi-layered midrib of thick-walled cells, and a lamina of rhomboidal cells that become more elongate toward the margin. The axes consist entirely of parenchyma with a central column of slightly smaller diam cells. Rhizoids are attached to the outer layer of the cortex and surround all the axes. These Permian fossils represent the oldest anatomically preserved bryophytes yet described from Gondwanaland and compare most closely with modern members of the Bryidae.     

STRUCTURALLY PRESERVED SPHENOPHYTES FROM THE TRIASSIC OF ANTARCTICA: VEGETATIVE REMAINS OF SPACIINODUM,GEN. NOV.

Sphenophyte remains of Early-Middle Triassic age are described from silicified peat collected in the Transantarctic Mountains of Antarctica. The new sphenophyte, Spaciinodum collinsonii sp. nov., is represented by ribbed, jointed stems with characteristic pith and carinal canals. Stems are relatively small, ranging from 1.8–3.0 mm in diameter, lack secondary tissues, and are characterized by vallecular canals that are restricted to nodal regions. The internodal vascular system consists of 12–18 collateral bundles which alternate between successive internodes. A complete vascular ring is present in the nodal region and is surrounded by a continuous double endodermis. Xylem is endarch and composed of elements ranging from annular to reticulate. The Antarctic sphenophyte is compared with other Gondwana fossil articulates and extant Equisetum. Superficial stomata suggest affinities with modern Equisetum subgenus Equisetum; however, some anatomical differences preclude assignment with living species.     

STRUCTURALLY PRESERVED LEAVES OF HARRIMANELLA HYPNOIDES (ERICACEAE): PALEOECOLOGY OF A NEW NORTH AMERICAN LATE PLEISTOCENE FOSSIL

Plant macrofossils from the basal inorganic sediments at Tom Swamp, north central Massachusetts, contained leaves, seeds, and fruits of arctic-alpine species, nearly all of which occur at present near the summits of Mt. Washington and Mt. Katahdin (New England) and in other alpine and arctic areas northward in eastern North America. Included were the needle-leaves of the dwarf shrub, Harrimanella hypnoides (L.) Coville, which matched comparative modern leaf samples in all anatomical details. The macrofossil assemblage was deposited before 12,830 ± 120 radiocarbon years ago and prior to the expansion of spruce populations in the region. Fossils of H. hypnoides suggest that snow beds were a regular feature of the summer landscape of southern New England during late glacial time. Calculations using the average lapse rate indicate that the mean annual paleotemperature in the Tom Swamp area may have been depressed 8–9 C below present means.     

10种卫矛科植物次生韧皮部的比较解剖

研究了卫矛科（Ｃｅｌａｓｔｒａｃｅａｅ）５ 属１０ 种植物次生韧皮部的结构。根据筛管分子、韧皮射线及厚壁组织的结构特征,将这１０ 种植物次生韧皮部分为３ 种类型。类型Ⅰ：筛管分子端壁倾斜,筛域数多,都为复筛板,韧皮射线大多为单列。卫矛属（Ｅｕｏｎｙｍ ｕｓ）的５ 种植物属于这一类型;类型Ⅱ：包括南蛇藤属（Ｃｅｌａｓｔｒｕｓ）和雷公藤属（Ｔｒｉｐｔｅｒｙｇｉｕｍ ）,其特征是筛管分子短,端壁倾斜度小,筛域数少,纤维不木质化,射线多列;类型Ⅲ：筛管分子多为单筛板,端壁接近水平,在不具功能韧皮部出现成簇的石细胞和纤维,射线单列或两列。属于此类型的有十齿花属（Ｄｉｐｅｎｔｏｄｏｎ）和核子木属（Ｐｅｒｒｏｔｔｅｔｉａ）     

ONTOGENY AND STRUCTURE OF THE SECONDARY PHLOEM IN EPHEDRA

The secondary phloem in Ephedra is atypical of the gymnosperms in general and exhibits several angiosperm-like characteristics. The ray system of the conducting phloem consists of parenchymatous, multiseriate rays. The axial system contains parenchyma cells, sieve cells, and unusual albuminous cells reminiscent of the specialized parenchyma cells found in some angiosperms. These cell types may intergrade with each other. P-protein in the developing sieve element appears early in the form of a single, ovoid slime body. Later, smaller slime bodies appear and quickly disperse. In the mature sieve element the single, ovoid slime body is lost, and P-protein is then evident in the form of a parietal cylinder, thread-like strands, amorphose globules, or a slime plug. Necrotic-appearing nuclei are commonly found in mature sieve cells.     

THE SEASONAL CYCLE OF PHLOEM DEVELOPMENT IN JUNIPERUS CALIFORNICA

In Juniperus californica, all sieve cells of the previous season's phloem growth increment overwinter in a mature state. Initiation of cambial activity begins in early March and, by the end of March, the oldest sieve cells that overwintered lose their contents and die. By mid-April, even the youngest sieve cells of the previous season's growth increment have lost their contents. The period of greatest cambial activity begins in the last half of April and continues through May. With the slowing of cambial activity in June, callose begins to collect on the sieve areas of the first-formed sieve cells of the new increment. By July, the cambium and phloem are in a dormant state. Initiation of phloem production precedes that of the xylem by about 1 month. Production of new xylem and phloem ceases simultaneously in July.     

SEASONAL DEVELOPMENT OF THE SECONDARY PHLOEM IN ACER NEGUNDO

Functional sieve elements are present year-round in the secondary phloem of the trunk of Acer negundo L., the box elder tree. Judging from numerous collections made between May, 1962, and May, 1964, the seasonal cycle of phloem development is as follows: cambial activity and new phloem differentiation begin in late March or early April; xylem differentiation begins about a month later and is completed in most trees in late August. At the time of cessation of cambial activity most of the relatively wide sieve elements of the current season's increment are mature. However, numerous groups of narrow, immature sieve elements and companion cells located on the outer margin of the cambial zone do not reach maturity until fall and winter. By the time of cambial reactivation in spring, most, if not all, of these narrow elements are mature. Some of the sieve elements which reach maturity either shortly after cessation of cambial activity or during dormancy become non-functional within 6 weeks after resumption of cambial activity in spring, while others remain functional until mid-August. For the phloem increment of a given year, cessation of function begins in September with the accumulation of definitive callose on the sieve plates of the first-formed sieve elements and spreads to all but the last-formed ones by the end of December.     

PROTEIN-CONTAINING CELLS IN THE NECTARY PHLOEM OF PASSIFLORA WARMINGII

Passiflora warmingii petiolar nectaries are characterized by the presence of large protein-containing phloem parenchyma cells which occupy the bulk of the nectary. Immature, mature, and senescent nectaries, as well as stem tips and petioles from unexpanded and mature leaves, were studied to learn the origin and fate of the protein and to determine if similar protein-containing cells occur in main-path phloem. The protein is present as membrane-limited fibrils in the phloem parenchyma of immature nectaries and in young main-path phloem. In the nectary, it persists until leaf senescence but becomes highly dispersed and barely detectable in mature main-path phloem parenchyma. Although superficially resembling P-protein it is always surrounded by a membrane, has smaller dimensions than is reported for P-protein, appears to be derived from RER, and is found in association with typical P-protein in the same cell. Possible functions for this material are suggested.     

DEVELOPMENT AND STRUCTURE OF PHLOEM IN THE PETIOLE OF LUFFA CYLINDRICA

Differentiation of external phloem is earlier than that of internal phloem in the young petiole of Luffa cylindrical. For a single sieve-tube element, one to six companion cells are present. The young sieve element shows many globular slime bodies which fuse longitudinally and disperse into the cytoplasm. Simultaneously the nucleus loses its stainable contents and later disorganizes. The contents of the sieve element are in the form of plugs, strands or a granular mass. Undispersed slime in the form of discrete bodies along the lateral walls is also observed. During one stage, at least, the dispersed slime and other contents of a mature sieve element lie at the periphery around a central cavity. A special type of phloem-parenchyma cell shows disorganizing chloroplasts, an extruded nucleolus, and callose on primary pit fields.     

STRUCTURALLY PRESERVED FOSSIL PLANTS FROM ANTARCTICA. I. ANTARCTICYCAS,GEN. NOV., A TRIASSIC CYCAD STEM FROM THE BEARDMORE GLACIER AREA

Silicified stems with typical cycadalean anatomy are described from specimens collected from the Fremouw Formation (Triassic) in the Transantarctic Mountains of Antarctica. Axes are slender with a large parenchymatous pith and cortex separated by a narrow ring of vascular tissue. Mucilage canals are present in both pith and cortex. Vascular tissue consists of endarch primary xylem, a narrow band of secondary xylem tracheids, cambial zone, and region of secondary phloem. Vascular bundles contain uni- to triseriate rays with larger rays up to 2 mm wide separating the individual bundles. Pitting on primary xylem elements ranges from helical to scalariform; secondary xylem tracheids exhibit alternate circular bordered pits. Traces, often accompanied by a mucilage canal, extend out through the large rays into the cortex where some assume a girdling configuration. A zone of periderm is present at the periphery of the stem. Large and small roots are attached to the stem and are conspicuous in the surrounding matrix. The anatomy of the Antarctic cycad is compared with that of other fossil and extant cycadalean stems.     

ANATOMY OF THE PRIMARY PHLOEM FIBER SYSTEM IN PISUM SATIVUM

Unusual structure of the primary phloem fiber system in the stem of Pisum sativum is described. The five lowest internodes contain large fiber strands that split radially and may also split tangentially. In both the stem and the root the number of fibers along a strand decreases with the distance below the leaf; in contrast, fiber length increases. Fiber dimensions are also increased in the centripetal direction.