Further studies of the sieve-element plastids of theCaryophyllales includingBarbeuia,Corrigiola, Lyallia,Microtea, Sarcobatus,andTelephium

The sieve-element plastids of 69 species of theCaryophyllales were investigated by transmission electron microscopy. All contained the specific subtype-P3 plastids characterized by a peripheral ring of protein filaments. The presence or absence of an additional central protein crystal and their shape being either polygonal or globular as well as the average sizes of the sieve-element plastids are useful features in the characterization of some families.—Barbeuia contains sieve-element plastids that confirm its placement within thePhytolaccaceae. Lyallia differs fromHectorella by including small starch grains in their sieve-element plastids, which otherwise by their globular crystals negate a closer connection to theCaryophyllaceae. The lack of a central protein crystal in its form-P3fs plastids placesMicrotea best within theChenopodiaceae. Sarcobatus, a so far uncontested member of theChenopodiaceae, contains form-P3cf plastids, i.e., including a central crystal not found elsewhere in this family.Telephium andCorrigiola, shifted back and forth betweenMolluginaceae andCaryophyllaceae, have form-P3cf(s) plastids with a polygonal crystal which favor their placement within theCaryophyllaceae.     

Sieve-Element Plastids,Nuclear Crystals and Phloem Proteins in the Zingiberales

The sieve-element characters of 40 species from all families making up the monocotyledon order Zingiberales have been studied by transmission electron microscopy. While phloem-proteins are a typical component of all eight families, the Zingiberaceae are characterized by nondispersive protein bodies derived from nuclear crystals. The sieve-element plastids are of the form-P2cs, i.e. contain cuneate protein crystals (as typical of all monocotyledons) and starch grains, those of the family Musaceae have protein filaments in addition (form-P2cfs). The exclusiveness of the form-P2c(f)s plastids contributed to the homogeneity of the order and its distinctness among other monocotyledon taxa. When diameters of the sieve-element plastids from leaf phloem are compared, in the “banana group” the family averages of the Strelitziaceae and the Lowiaceae have, respectively, maximum and minimum values and are clearly different from those in the Musaceae, the family in which they have been included previously. In the “ginger group”, the family averages of the Zingiberaceae, Costaceae, and Marantaceae are close to the order average, with only Cannaceae having minimum values. A comparison of species averages, however, reduces the size differences between families: the value for Ravenala (Strelitziaceae) is close to those of the five Musaceae tested, and that of Globba (Zingiberaceae) even slightly lower than the species average of Canna.     

P-type sieve-element plastids and the systematics of theArales (sensuCronquist 1988)—with S-type plastids inPistia

The sieve-element plastids of 126 species of theArales were investigated by transmission electron microscopy. With the exception ofPistia (with S-type plastids) all contained the monocotyledon specific subtype-P2 plastids characterized by cuneate protein crystals. While the species studied from bothAcoraceae andLemnaceae have form-P2c plastids (i.e., with cuneate crystals only), those of theAraceae belong to either form P2c (14 species), P2cs (the great majority) or P2cfs (Monstera deliciosa, only, with form-P2cs plastids in the otherMonstera species studied). The form-P2cs plastids of theAraceae are grouped into different categories according to the quantity and quality of their protein and starch contents. The subfamilyLasioideae is redefined to comprise all aroid P2c-taxa and those P2cs-genera that contain only one or very few starch grains. Only little starch is also recorded in the sieve-element plastids ofGymnostachys (Gymnostachydoideae), with the other plastid data denying a close relationship toAcorus. While equal amounts of starch and protein are generally present in sieve-element plastids of the subfamiliesPothoideae, Monsteroideae, Colocasioideae, Philodendroideae, andAroideae, maximum starch content and only very few protein crystals are found in form-P2cs plastids ofCalla (Calloideae),Ariopsis (Aroideae), andRemusatia (Colocasioideae?). In the latter, both morphology and size of sieve-element plastids are close to those ofPistia.—In theAraceae the diameters of the sieve-element plastids exhibit a great size range, but are consistent within a species and within a defined part of the plant body. Comparative data are mainly available for stem and petiole sieve-element plastids.—The accumulated data are used to suggest an affiliation of the species to subfamilies and to discuss the phylogeny of theArales. Forms and sizes of their plastids support a separation of bothAcoraceae andLemnaceae from theAraceae. The presence of S-type plastids inPistia does not favour direct and close relationships to the form-P2c genusLemna.—The prevailing form-P2cs plastids might support proposals that place theArales (together with also form-P2cs plastid containingDioscoreales) in the neighbourhood of basal dicotyledons. BesidesAsarum andSaruma (Aristolochiaceae), with monocotyledonous form-P2c plastids,Pistia (with dicotyledonous S-type plastids) gives another example for a link between the two angiosperm classes.     

Ultrastructure of sieve-element plastids inCaryophyllales (Centrospermae), evidence for the delimitation and classification of the order

The orderCaryophyllales (Centrospermae) was found to contain specific P-type sieve-element plastids which are characterized by protein inclusions composed of ring-shaped bundles of filaments and of central crystalloids. The sieve-element plastids of 14 families (140 species investigated) fit into this overall characterization, and more specific details are used to delimit the families and arrange them within the order.Phytolaccaceae, the basic family of the order display much diversity: the crystalloids inside their plastids are either globular (most genera) or polygonal (Stegnosperma), starch may also be present (Phytolacca).Nyctaginaceae, with starch inBougainvillea sieve-element plastids, can be derived directly fromPhytolacca. Globular crystalloids are present in most of the families, as inDidiereaceae, Cactaceae, Aizoaceae-Tetragoniaceae, Portulacaceae-Basellaceae-Halophytaceae-Hectorellaceae. Caryophyllaceae andLimeum ofMolluginaceae contain polygonal crystalloids (otherMolluginaceae with globular crystalloids). Crystalloids are entirely absent fromChenopodiaceae (incl.Dysphaniaceae) andAmaranthaceae. The probable relationships between these families are presented diagrammatically in Fig. 13. Bataceae, Gyrostemonaceae, Vivianiaceae, Theligonaceae, Polygonaceae, Plumbaginaceae, Fouquieriaceae, Frankeniaceae, andRhabdodendraceae—all at some time included into theCaryophyllales (Centrospermae) or doubtfully referred to them—develop S-type (or different P-type) sieve-element plastids. Their direct connection to theCaryophyllales therefore is excluded. Finally, evolutionary trends of theCaryophyllales are discussed.Presented in the Symposium Evolution of Centrospermous Families, during the XIIth International Botanical Congress, Leningrad, July 8, 1975.     

Sieve-element plastids ofCyrillaceae,Erythroxylaceae andRhizophoraceae: Description and significance of subtype PV plastids

A new subtype (PV) of protein-containing sieve-element plastids was found to contain a uniquely large number of polygonal protein crystals, sometimes with (PVcf) and sometimes without (PVc) protein filaments. These plastids do not accumulate starch. The PVcf-plastids occur inCyrillaceae only, while the PVc-plastids are limited toErythroxylaceae andRhizophoraceae. The significance of the new P-subtype with respect to the systematic position of the three families is discussed.     

Contributions to the knowledge of sieve-element plastids inGunneraceae and allied families

P-type sieve-element plastids were found in theGunneraceae, while S-type plastids are present in theHaloragaceae andHippuridaceae. The specific characters of the sieve-element plastids (e.g., their size and the morphology of their contents) are discussed in relation to other taxa of theRosidae containing P-type plastids and to the systematic position of theGunneraceae. Contributions to the Knowledge of P-Type Sieve-Element Plastids in Dicotyledons, III. — For other parts of this series see (I.:)Behnke (1982 b) and (II.:)Behnke (1985).     

Sieve-element plastids ofGymnospermae: Their ultrastructure in relation to systematics

The distribution of S-type and P-type plastids in the sieve elements of 30 species from 13 families of theConiferophytina andCycadophytina is recorded, of which 21 species were studied for the first time with respect to their sieve-element plastids. While starch storing S-type plastids are the most commonly occurring type throughout both taxa, all thePinaceae examined (11 species of 7 genera) contain P-type plastids characterized by a peripheral, ring-shaped bundle of protein filaments, an additional protein crystalloid, and several starch grains. Starch grains of sieve-element plastids in theConiferophytina andCycadophytina are commonly club-shaped. Taxonomic implications of these ultrastructural findings on sieve-element plastids are discussed.     

P-type sieve-element plastids present in members of the tribesTriplareae andCoccolobeae (Polygonaceae) renew the links between thePolygonales and theCaryophyllales

Form-Pfs sieve-element plastids were found inTriplaris, Ruprechtia, andCoccoloba (Polygonaceae) while other genera of the family and those studied from the often associatedPlumbaginaceae contain S-type sieve-element plastids. The rareness of form-Pfs plastids among the angiosperms, their similarity to the peculiar form-P3fs plastids of theChenopodiineae, and the comparatively small plastid diameters measured for all forms present in theCaryophyllales, Polygonales, andPlumbaginales suggest close relationships between these taxa. The restriction inPolygonaceae of form-Pfs plastids to the closely allied tribesTriplareae andCoccolobeae is discussed with regard to both the intrafamilial and ordinal phylogeny, and also considering possible connections to the only magnoliidaean Pfs-taxonCanella. Dedicated to Univ.-Prof. DrF. Ehrendorfer on the occasion of his 70th birthday.     

Sieve-element plastids,exine sculpturing and the systematic affinities of theBuxaceae

The sieve-element plastids of members of several genera in theBuxaceae (Buxus, Pachysandra andSarcococca) were found to be of the specific subtype PVI, which contains a central globular protein crystal.Simmondsia (Simmondsiaceae) andDaphniphyllum (Daphniphyllaceae), on the other hand, were found to contain S-type sieve-element plastids. The occurrence of the highly restricted PVI plastids in theBuxaceae mitigates against a close relationship between theBuxaceae andSimmondsia, Daphniphyllum andEuphorbiaceae. Exine sculpturing of theBuxaceae andSimmondsiaceae also shows no close similarities. Both of these EM characters are discussed in connection with other available data and with respect to earlier systematic treatment of these families.     

Form-Pfs Plastids,Stem Anatomy and Systematic Affinities of Stylobasium Desf. (Stylobasiaceae)

The vascular system of the stem of Stylobasium was investigated during its primary and secondary phases with both light and electron microscopic methods. It contains collateral bundles arranged in a ring, separated by rays which undergo regular cambial growth. The phloem consists of short sieve elements connected to sieve tubes by simple sieve plates, companion cells of the same length, and phloem parenchyma cells. During their autophagy-like differentiation and maturation, typical of all angiosperms, the sieve elements of Stylobasium have a peculiar feature, whereby they develop and retain form-Pfs plastids (containing protein filaments and starch). The sieve-element plastids of the two Stylobasium species, and of some 100 species belonging to taxa of which Stylobasium had been considered to be a possible member, have been studied by transmission electron microscopy. With the exception of a few species with form-Pcs plastids (containing a single small protein crystal in addition to starch), the great majority of taxa studied are characterized by S-type sieve-element plastids (containing starch only). The presence of form-Pfs plastids in Stylobasium supports its separation into the unigeneric Stylobasiaceae and the placement of this family close to other form-Pfs or form-Pcfs-containing taxa. While other characters would exclude an affiliation to the Magnolianae (form-Pfs plastids in Canella) or Caryophyllales (form-Pfs plastids in Microtea), an association with the form-Pcfs families Connaraceae and Mimosaceae is positively considered and corresponds to their frequent allocation close to the Rutales and Sapindales. Within the Rutales/Sapindales the sizes of sieve-element plastids (average diameter) range from very large (e.g. in the Julianaceae) to comparatively small (e.g. in Aceraceae) and are used to group the families. The sieve element characters of the Coriariaceae (tiny plastids with almost no starch, wide sieve plate pores, copious P-protein) suggest their removal from Rutales/Sapindales into the neighbourhood of the Cucurbitaceae.     

Sieve-Element Characters of the Proteaceae and Elaeagnaceae: Nuclear Crystals,Phloem Proteins and Sieve-Element Plastids

The sieve-element characters of 34 species from the Proteaceae and Elaeagnaceae have been studied by transmission electron microscopy. While nondispersive protein bodies and dispersive P-protein are typical components of both families, specific forms and/or their distinctive origin accentuate some taxa. Within the Grevilloideae, subfamily of Proteaceae, a number of Australian species and genera contain protein crystals of nuclear origin arranged into rosette-like bodies, while in the other members studied from the same subfamily no nondispersive protein bodies were found. Several Australian and South African genera of the Proteoideae contain compound-spherical nondispersive protein bodies that reside in the cytoplasm from their very beginning. In the Elaeagnaceae three different P-protein bodies are present of which one is tubular and dispersing, another is nondispersive and of irregular-stellate form, and a third is globular (resembling a P-protein from Cucurbita). The great majority of the species studied from the Proteaceae contains form-Ss sieve-element plastids, Lomatia ilicifolia and Macadamia ternifolia are distinct in having form-Pcs plastids. The average diameter of stem sieve-element plastids in the family is 1.38 μm. The Elaeagnaceae (three species investigated) is a pure form-So family (average diameter: 0.8 μm). There are no specific sieve-element characters that would support any relationship between the Proteaceae and Elaeagnaceae. While affinities of the former to pre-Gondwanan parts of the Rosanae/Myrtanae are discussed, a reconsideration of the Elaeagnaceae as a possible member of the Violanae (identical features with Cucurbitaceae) is proposed.     

Elektronenmikroskopische Untersuchungen zur Frage der verwandtschaftlichen Beziehungen zwischenTheligonum undRubiaceae: Feinbau der Siebelement-Plastiden und Anmerkungen zur Struktur der Pollenexine

Theligonum cynocrambe and 13 species ofRubiaceae contain S-type sieve-element plastids, wide-spread in Dicotyledons. Alignment ofTheligonum toCaryophyllales (Centrospermae), especiallyPhytolaccaceae, is unlikely, because this order is characterized by specific P-type plastids. SEM investigations show the pollen exine ofTheligonum to be microreticulate, with additional supratectate spinules.Asperula and other genera of the tribeRubieae have a tectum perforatum (punctitegillate sexine), also with supratectate verrucae or spinulae.—Thus ultrastructure suggests (but not definitely proves) relationships betweenTheligonum andRubiaceae, while affinities betweenTheligonum andCaryophyllales are excluded.

     

Recircumscription of the monocotyledonous family Petrosaviaceae to include Japonolirion

Most systematists have favored placing Petrosaviaceae close to the Triuridaceae (formerly positioned within Alismatidae) by focusing on the mycoheterotrophic habit and nearly free carpels of Petrosaviaceae. Others have favored a position near the melanthioid lilies, perhaps serving as a linking-family to the Triuridaceae. We discuss the results of recently published, independent, and combined DNA sequence analyses that indicate a strongly supported sister relationship betweenPetrosavia (Petrosaviaceae) andJaponolirion (Japonoliriaceae). Molecular data show no connection of these genera to the Alismatales (including Tofieldiaceae), the Melanthiaceae s. str., the Liliales, or the Triuridaceae (now in Pandanales), although there are morphological similarities to each of these groups. A relationship to the Pandanales has been indicated in some molecular analyses, but this is not supported by bootstrap/jackknife analyses or by most morphological characters. BothPetrosavia andJaponolirion are native to high-evelation habitats and have bracteate racemes, pedicellate flowers, six persistent tepals, septal nectaries, three nearly distinct carpels, simultaneous microsporogenesis, monosulcate pollen, and follicular fruits. Outside of the Alismatales, no other monocotyledons share this combination of features. We therefore suggest that the Petrosaviaceae be re-circumscribed to includeJaponolirion. If the family's isolated position among the monocot orders continues to be found in phylogenetic studies, then recognition of the already published order Petrosaviales would be appropriate.     

S-type sieve-element plastids and anthocyanins inVivianiaceae: Evidence against its inclusion intoCentrospermae

The presence of S-type sieve-element plastids and anthocyanins in theVivianiaceae indicates that it is not a member ofCentrospermae (Caryophyllales).     

Ultrastructural,micromorphological and phytochemical evidence for a “Central Position” ofMacarthuria (Molluginaceae) within theCaryophyllales

Subtype PIII sieve-element plastids, anthocyanins, spinulose, perforate-tectate pollen grains and the specific seed-coat sculpturing found in twoMacarthuria species (M. australis, M. neocambrica) consolidate their placement withinMolluginaceae. The unique form of the sieve-element plastids, i.e. with cubic crystals and starch grains (PIIIc″fs), finds its closest counter-part inLimeum. The multiple intertwinement of different genera of theMolluginaceae with many other centrospermous families led to a consideration of their more central position withinCaryophyllales.     

Die Siebröhren-Plastiden der Monocotyledonen

Zusammenfassung In vergleichenden feinstrukturellen Beobachtungen an 24 Monocotyledonen aus 21 Familien wird ein für Monocotylen-Siebröhren charakteristischer Plastidentyp näher beschrieben. Neben gelegentlichen Ablagerungen von Siebröhrenstärke enthalten ausdifferenzierte Siebröhren-Plastiden zahlreiche keilförmige, kontrastreiche und proteinhaltige Kristalloide. Sie entstehen in der Matrix der noch amöboiden Formveränderungen unterworfenen Proplastiden; in reifem Zustand werden sie aus gekreuzten Reihen paralleler, gerader und kontrastreicher Filamente (50–60 Å) aufgebaut.Die Siebröhren-Plastiden von Nymphaea alba und Nuphar luteum bilden keine Kristalloide aus, dagegen läßt sich Siebröhrenstärke wie in den übrigen bisher untersuchten Dicotylen nachweisen.

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Sieve-tube plastids of monocotyledonsComparative investigations of the fine structure and distribution of specific plastids

Summary Fine-structural investigations of 24 monocotyledons from 21 families and all but one order succeeded in revealing a plastid with cuneate proteinaceous inclusion bodies as being typical of monocot sieve-tubes. Inclusion bodies originate in large numbers during plastid differentiation; they concentrate in the matrix and aggregate around an invisible centre, that mostly lies at one end of the elongated ameboid proplastid. The inclusion-free part of the young plastid contains countless vesicles and short membranes, presumably invaginations of the inner plastid envelope. Proteinaceous inclusion bodies show a crystal-like structure composed of 50–60 Å subunits in straight and parallel order. Besides these crystal-like inclusion bodies sieve-tube plastids of many monocotyledons also contain starch. — Sieve-tube plastids of Nuphar luteum and Nymphaea alba look like plastids in dicotyledon sieve-tubes, starch being their only inclusion.

     

Plastids of sieve tube members in the stamen vascular bundle ofSorghum bicolor (Gramineae)

Summary The plastids in sieve tube members of the stamen vascular bundles ofSorghum bicolor, fixed in glutaraldehyde with postfixation in osmium tetroxide, are of the P-type containing cuneate crystalloids of a proteinaceous nature surrounded by a double envelope. Secondary inclusions are present in these P-type plastids. P-type plastids inSorghum often remain intact in the mature sieve tube members.This work was supported by a grant from the Iowa Agricultural and Home Economics Experiment Station, Ames, U.S.A. Project No. 1740 toHarry T.Horner, Jr., andNels R.Lersten and Project No. 1914 toHarry T.Horner, Jr. of the Department of Botany and Plant Pathology, Iowa State University, Ames, U.S.A. This work was completed by the author as part of the Ph. D. dissertation research.     

Starch-accumulating (S-type) sieve-element plastids in Hydatellaceae: implications for plastid evolution in flowering plants

TEM investigation of sieve-element plastids in three species of Trithuria, the sole genus of the small aquatic family Hydatellaceae, show that P-type plastids are absent from this genus and only starch-accumulating (S-type) sieve-element plastids are present. This discovery is consistent with the recent transfer of Hydatellaceae from the highly derived monocot order Poales (grasses and their allies) to the early-divergent angiosperm order Nymphaeales (waterlilies) based on molecular phylogenetic data. Species of Poales consistently possess P2-subtype plastids, in common with other monocots, but only S-type plastids are present in Nymphaeales. The results confirm that Hydatellaceae do not belong in monocots. Optimisation of the two major types of sieve-element plastid onto a recent phylogeny of early-divergent angiosperms confirms that S-type is the primitive form and indicates that P-type sieve-element plastids have evolved more than once in angiosperms.     

ULTRASTRUCTURAL FEATURES OF DEVELOPING SIEVE ELEMENTS IN LEMNA MINOR L.—THE PROTOPLAST

The occurrence and precise arrangement of phloem tissue is reported for the first time in the root of the duckweed, Lemna minor L. Since these plants are small enough to be prepared intact for electron microscopy, the induction of artifacts as a result of mechanical manipulation during specimen preparation is virtually eliminated. Ultrastructural features of the complete sequence of sieve-element development are presented and are in some respects similar to what has been described in other monocotyledons (e.g., nuclear degeneration, aggregation of ER, elaboration of electron-dense crystalline plastid inclusions). Mature sieve elements in Lemna are enucleate, lack P-protein, contain a plasmalemma, ER-aggregations, mitochondria, plastids and, in many instances, intact vacuoles. It is suggested that structural modification required for the sieve element to assume a transport function may not be very drastic, apart from the degeneration of the nucleus.     

Refractive spherules in phloem ofMicrosorium scolopendria andPsilotum nudum

Summary Phloem tissues ofMicrosorium scolopendria (Polypodiaceae) andPsilotum nudum (Psilotaceae) were examined with light and electron microscopes. The characteristic refractive spherules in the sieve elements ofM. scolopendria apparently develop from endoplasmic reticulum-derived cytoplasmic vesicles. In both taxa they have not been observed to be spatially related to plastids or mitochondria. Refractive spherules contain protein and often occur in the peripheral cytoplasm of mature sieve elements. InM. scolopendria they also occur in pericycle cells. Significant differences in refractive spherule substructure occur between the two taxa studied.