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Journal ArticleDOI

Anatomy of the Dicotyledons.

About: This article is published in American Midland Naturalist.The article was published on 1950-11-01. It has received 2511 citations till now.
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Journal ArticleDOI
TL;DR: Evidence for the conservation of CaOx crystals in cotyledons during the L. miyakojimae germination process was supported by the biochemical measurement of oxalic acid levels.
Abstract: The cotyledon of legume seeds is a storage organ that provides nutrients for seed germination and seedling growth. The spatial and temporal control of the degradation processes within cotyledons has not been elucidated. Calcium oxalate (CaOx) crystals, a common calcium deposit in plants, have often been reported to be present in legume seeds. In this study, micro-computed tomography (micro-CT) was employed at the SPring-8 facility to examine the three-dimensional distribution of crystals inside cotyledons during seed maturation and germination of Lotus miyakojimae (previously Lotus japonicus accession Miyakojima MG-20). Using this technique, we could detect the outline of the embryo, void spaces in seeds and the cotyledon venation pattern. We found several sites that strongly inhibited X-ray transmission within the cotyledons. Light and polarizing microscopy confirmed that these areas corresponded to CaOx crystals. Three-dimensional observations of dry seeds indicated that the CaOx crystals in the L. miyakojimae cotyledons were distributed along lateral veins; however, their distribution was limited to the abaxial side of the procambium. The CaOx crystals appeared at stage II (seed-filling stage) of seed development, and their number increased in dry seeds. The number of crystals in cotyledons was high during germination, suggesting that CaOx crystals are not degraded for their calcium supply. Evidence for the conservation of CaOx crystals in cotyledons during the L. miyakojimae germination process was also supported by the biochemical measurement of oxalic acid levels.

17 citations

Journal ArticleDOI
TL;DR: The ontogenesis, structure, ultrastructure and histochemical aspects of the protuberances in Cissus verticillata, which have been described since the beginning of the 19th century as pearl glands or pearl bodies, are examined in order to establish a relationship between their structure and function.

17 citations


Cites background from "Anatomy of the Dicotyledons."

  • ...The structures previously described as pearl glands in Cissus verticillata (see Solereder, 1908; Metcalfe and Chalk, 1979) act as FBs, being capable of recruiting ants by offering them sugar and oil rewards....

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Journal ArticleDOI
TL;DR: Analysis support the use of Tillandsia usneoides as a wide biomonitor of air quality in urbanized areas based on chemical and structural markers to detect changes in air quality.
Abstract: Tillandsia usneoides is an aerial epiphytic bromeliad that absorbs water and nutrients directly from the atmosphere by scales covering its surface. We expanded the use of this species as a broader biomonitor based on chemical and structural markers to detect changes in air quality. The usefulness of such comprehensive approach was tested during the construction and opening of a highway (SP-21) in Sao Paulo State, Brazil. The biomonitoring study was performed from 2009 to 2012, thus comprising the period during construction and after the highway inauguration. Metal accumulation and structural alterations were assessed, in addition to microscopy analyses to understand the metal chelation in plant tissues and to assess the causes of alterations in the number and shape of scale cells. Altogether, our analyses support the use of this species as a wide biomonitor of air quality in urbanized areas.

17 citations


Cites methods from "Anatomy of the Dicotyledons."

  • ...The scale index was calculated over the stomatal density formula (Salisbury 1927 apud Metcalfe and Chalk 1979): number of scales / number of epidermal cells + number of scales × 100....

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Journal ArticleDOI
TL;DR: Seed morphology and leaf epidermal features of 22 species of Schisandraceae are studied in order to provide additional data for a morphological data matrix and do not yield further evidence for monophyly of the two genera.
Abstract: Schisandraceae are traditionally subdivided in two genera, Schisandra and Kadsura, based on differences in the organisation of the floral receptacle, the carpels, and the presence or absence of a ``pseudostigma''. Recently, phylogenetic analyses utilizing ITS sequence data and morphological data resulted in incongruent tree topologies, with the morphological trees suggesting monophyly of the two genera, whereas ITS trees did not resolve Schisandra and Kadsura as monophyletic clades. In the present paper we study seed morphology and leaf epidermal features of 22 species of Schisandraceae in order to provide additional data for a morphological data matrix. Seed morphological characters are highly homoplastic and do not yield further evidence for monophyly of the two genera. Instead, a number of characters appear to support sister group relationships between taxa within the genera, such as, for instance, for K. coccinea and K. scandens, both of which have large seeds along with a multi-layered mesotesta. Considering leaf epidermal characteristics, species of Kadsura were found to be consistently amphistomatic, whereas species of Schisandra are always hypostomatic. Phylogenetic analysis using the extended data matrix resulted in weakly supported Kadsura and Schisandra clades with five and four synapomorphies indicating monophyly of Kadsura and Schisandra, respectively. Fossils ascribed to Schisandraceae date back to the Late Cretaceous. These are tri-and hexacolpate pollen types displaying a combination of features found in modern Schisandraceae and partly also in Illiciaceae. Leaf remains from this period are poorly preserved and difficult to ascribe to Schisandraceae because of the lack of synapomorphies for the family. In the Early Cainozoic, leaf and seed remains from North America and Europe unambiguously belong to the family. Seeds from the Eocene of North America show some similarities to the modern Schisandra glabra from North America, while fossils from Europe show more similarities to modern Asian species.

17 citations