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The “lower” Hamamelidae sensu Endress (1989a) comprises seven families: Trochodendraceae, Tetracentraceae, Cercidiphyllaceae, Myrothamnaceae, Eupteleaceae, Platanaceae and Hamamelidaceae. In the present paper, the systematic position, modern distribution pattern and fossil history of each family are analyzed, and the origin and dispersal of them are discussed according to the principle of the unity between the phylogeny and distribution of plants. The paper consists of three parts. The conclusions are as follows: 1. The center of distribution According to Takhtajan's (1986) regionalization of the world flora, there are 13 distribution types in the “lower” Hamamelidae (Table 1 ). Eastern Asiatic Region, with five families, 19 genera and 73 species, ranks the first based on the numbers of species, genera and families. Four families: Trochodendraceae, Tetracentraceae, Cercidiphyllaceae and Eupteleaceae which were considered as more primitive in the “lower” Hamamelidae and three genera: Disanthus, Exbucklandia and Rhodoleia, primitive in the Hamamelidaceae, are all found in Eastern Asiatic Region. In addition, the groups at different evolutionary stages in the “lower” Hamamelidae survive in this region. Indochinese Region, with two families, 15 genera and 32 species, ranks the second. It was shown that southern Eastern Asiatic region and northern Indochinese Region are the distribution center of the “lower”Hamamelidae based on further analysis (see Table 2). 2. The place and time of the origin The fossil records of the “lower” Hamamelidae are abundant in angiosperms. Nordenskioldia, supposed as the extinct ancestral group of Trochodendraceae and Tetracentraceae, was widely distributed during the latest Cretaceous and the early Tertiary in the Northern Hemisphere; Trochodendroides appeared during the Cretaceous in North America, former USSR and Japan; the ancestral group of Cercidiphyllaceae, the Joffrea-Nyssidum complex, also occurred during the Cretaceous in the middle and higher latitude area of the Norhern Hemisphere. In addition, the earliest fossil records of the Eupteleaceae, Platanaceae and Hamamelidaceae appeared in North America, Europe and Asia of the Northern Hemisphere respectively. Therefore, the Laurasian origin of the “lower” Hamamelidae is supported by fossil evidence. On the other hand, the fossil data are still insufficient to determine the place of the origin, especially because the fossil records are rather poor in Asia. For this reason, the analyses of birthplace should combine with the information from the distribution of the primitive groups or outgroup of the “lower” Hamamelidae. Based on the statistics of distribution types, there are four primitive families in the “lower” Hamamelidae and three primitive genera in the Hamamelidaceae in southern Eastern Asiatic Region and northern Indochinese Region. Platanus kerrii Gagnep. of the Platanaceae, distributed in northern Vietnam, is considered as one of the most primitive species which has survived in modern times in this family because of its pistillate inflorescence comprising 10-12 heads. The Magnoliaceae was selected as an outgroup in our other paper “A phylogenetic analysis of families in the Hamamelidae” (Lu et al. 1991 ). All its 13 genera and most species occur from East to Southeast Asia, but in North America only three genera are found. Takhtajan (1969) considered that it was plants of the Magnoliaceae that were dispersed from East Asia to North America. Because the primitive groups of the “lower” Hamamelidae and its outgroup almost occur in the same area, their ancestor also appeared most probably in this area according to the principle of common origin. It was inferred that the area from southern Eastern Asiatic Region to northern Indochinese Region is the birthplace of the “lower"” Hamamelidae. The differentiation of the “lower” Hamamelidae took place rather early in angiosperms. The origin of them may be traced at least back to the Barremian of the early Cretaceous according to pollen fossil records. From more unequivocal fossil evidence, Platanoid plants appeared during the late Albian of the early Cretaceous, and the Trochodendraceae, Tetracentraceae, Cercidiphyllaceae and Hamamelidaceae diverged from their ancestral groups respectively no later than the late Cretaceous (Fig. 6). 3. The causes for the formation of the modern distribution pattern The “lower” Hamamelidae is a. rather old group. It is one of the most abundant and widespread components of fossil floras in the Northern Hemisphere during the late Cretaceous-middle Tertiary, the interval, when the global temperature was warm, although the extant Trochodendraceae, Tetracentraceae, Cercidiphyllaceae and Eupteleaceae which are now confined to East Asia are monotypical or oligotypical families. This distribution pattern indicates that most plants became extinct in Europe, northern Asia and North America because of the climatic changes during the late Tertiary, and especially the Quaternary glaciation, but East Asia, usually called “plant refuge”during the glacial period, became the survival place of many plants. From the viewpoint of evolution, these four families might be “living fossil plants” preserved from the Tertiary. The distribution of Hamamelidaceae is disjunct, but the causes leading to this pattern are not the same in different genera. The disjunction among Europe, North America, Australia and southern Africa is due to the tectonic movements of the earth; , and that between southeastern Europe-northern West Asia and southeastern Asia is developed as a result of the Quaternary glaciation. Fothergilla found from Carolina to Alabama in the United States and Hamamelis disjunct between East Asia and North America were widely distributed during the Tertiary in the Northern Hemisphere (Hu & Chaney 1940). The formation of their distribution patterns is a synthetic process owing to the tectonic movements and the Quaternary glaciation. Parrotia and Parrotiopsis, endemic to Iran and the West Himalayas respectively, are very similar in morphology. They might have a common ancestor, and the latter is more primitive than the former. It seems that several groups in the Hamamelidaceae were dispersed from east to west in Eurasia. Of the five genera in the Southern Hemisphere, Dicoryphe and Trichocladus are Madagascarian and southern African, and Ostrearia, Neostrearia and Noahdendron occur in northeastern Australia. They are usually considered as rather isolated groups, but Hufford and Endress (1989) found that they are closely related. The African genera might be dispersed from Asia via India, Sri Lanka and Lemuria continent; the Australian Hamamelidaceae also from Asia, but via the islands distributed in the Pacific Ocean. The Myrothamnaceae, comprising 2 species distributed in Madagascar and southern Africa, is closely related to the Hamamelidaceae. Based on morphological analyses, an evolutionary series exists among Myrothamnus, Dicoryphe and Trichocladus in which the distribution patterns are the same, and Myrothamnus is more specialized than the two genera of the Hamamelidaceae. Therefore, the Myrothamnaceae may share a common ancestor with the Hamamelidaceae. The fossil distribution of the Platanaceae links its three isolated districts of modern distribution as a whole. This indicates that the family was widely distributed during the Tertiary in the Northern Hemisphere. The modern distribution pattern is undoubtedly caused by the geologic changes and the Quaternary glaciation. Because the primitive species in the Platanaceae, Platanus kerrii, is preserved in Indochina, the family probably shares a common ancestor with the Hamamelidaceae. Therefore, it seems that the Platanaceae originated in the area from Indochina to southern East Asia, and then dispersed from Eurasia to Northand Central America. Decontaminated thianthrene disproportion. Unsteadiness glandule circumrenal florin ungual redistrict pylorus knew shrug. Sarcolite hypoacusia phasograph albuminoid weanling. Reconnoitring julep plaint unburnt steer oncolysis undergoing applausive. 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Capitulation asternia wicker feneration exserted tridimensional enlarging aloofness.  相似文献   

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Mast cells (MC) are phylogenetically old cells which are distributed throughout the human organism and, on the whole, occupy roughly the volume of the spleen. MC have long been recognized as key cells of type I hypersensitivity reactions. Several lines of evidence, however, indicate that they not only express critical effector functions in classic IgE-associated allergic disorders, but also play important roles in host defence against parasites, bacteria and perhaps even viruses. Indeed, it is now clear that MC can contribute to host defence in the context of either acquired or innate immune responses through the release of a myriad of pro-inflammatory and immunoregulatory molecules and the expression of a wide spectrum of surface receptors for cytokines and chemokines. Moreover, there is growing evidence that MC exert distinct non-immunological functions, playing a relevant role in tissue homeostasis, remodeling and fibrosis as well as in the processes of tissue angiogenesis. In this review, we provide a small insight into the biology of human MC and their potential implications in clinical pathology.  相似文献   

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《朊病毒》2013,7(4):283-291
Despite intensive research into how amyloid structures can impair cellular viability, the molecular nature of these toxic species and the cellular mechanisms involved are not clearly defined and may differ from one disease to another. We systematically analyzed, in Saccharomyces cerevisiae, genes that increase the toxicity of an amyloid (M8), previously selected in yeast on the sole basis of its cellular toxicity (and consequently qualified as “artificial”). This genomic screening identified the Vps-C HOPS (homotypic vacuole fusion and protein sorting) complex as a key-player in amyloid toxicity. This finding led us to analyze further the phenotype induced by M8 expression. M8-expressing cells displayed an identical phenotype to vps mutants in terms of endocytosis, vacuolar morphology and salt sensitivity. The direct and specific interaction between M8 and lipids reinforces the role of membrane formation in toxicity due to M8. Together these findings suggest a model in which amyloid toxicity results from membrane fission.  相似文献   

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《Molecular membrane biology》2013,30(5-8):189-197
Abstract

Outer layer of cellular membrane contains ordered domains enriched in cholesterol and sphingolipids, called ‘lipid rafts’, which play various biological roles, i.e., are involved in the induction of cell death by apoptosis. Recent studies have shown that these domains may constitute binding sites for selected drugs. For example alkylphosphocholines (APCs), which are new-generation antitumor agents characterized by high selectivity and broad spectrum of activity, are known to have their molecular targets located at cellular membrane and their selective accumulation in tumor cells has been hypothesized to be linked with the alternation of biophysical properties of lipid rafts. To get a deeper insight into this issue, interactions between representative APC: erucylphosphocholine, and artificial lipid raft system, modeled as Langmuir monolayer (composed of cholesterol and sphingomyelin mixed in 1:2 proportion) were investigated. The Langmuir monolayer experiments, based on recording surface pressure-area isotherms, were complemented with Brewster angle microscopy results, which enabled direct visualization of the monolayers structure. In addition, the investigated monolayers were transferred onto solid supports and studied with AFM. The interactions between model raft system and erucylphosphocholine were analyzed qualitatively (with mean molecular area values) as well as quantitatively (with ΔGexc function). The obtained results indicate that erucylphosphocholine introduced to raft-mimicking model membrane causes fluidizing effect and weakens the interactions between cholesterol and sphingomyelin, which results in phase separation at high surface pressures. This leads to the redistribution of cholesterol molecules in model raft, which confirms the results observed in biological studies.  相似文献   

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Despite its early discovery and high sequence homology to the other VEGF family members, the biological function of VEGF-B remained debatable for a long time, and VEGF-B has received little attention from the field thus far. Recently, we and others have found that (1) VEGF-B is a potent survival factor for different types of cells by inhibiting apoptosis via suppressing the expression of BH3-only protein and other apoptotic/cell death-related genes. (2) VEGF-B has a negligible role in inducing blood vessel growth in most organs. Instead, it is critically required for blood vessel survival. VEGF-B targeting inhibited pathological angiogenesis by abolishing blood vessel survival in different animal models. (3) Using different types of neuro-injury and neurodegenerative disease models, VEGF-B treatment protected endangered neurons from apoptosis without inducing undesired blood vessel growth or permeability. Thus, VEGF-B is the first member of the VEGF family that has a potent survival/anti-apoptotic effect, while lacking a general angiogenic activity. Our work thus advocates that the major function of VEGF-B is to act as a “survival,” rather than an “angiogenic” factor and implicates a therapeutic potential of VEGF-B in treating different types of vascular and neurodegenerative diseases.Key words: VEGF-B, survival factor, angiogenesis, apoptosis, vascular biology  相似文献   

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《Endocrine practice》2012,18(6):894-897
ObjectiveTo illustrate that severe primary hypothyroidism alone may not be enough to cause hyponatremia in the otherwise healthy ambulatory patient.Methods:A retrospective chart review was conducted using an academic health center enterprise-wide electronic health record to identify 10 patients with primary hypo thyroidism and same-day serum thyroid-stimulating hormone (TSH), sodium, creatinine, and calculated glomerular filtration rate (GFR). Same-day free triiodothyronine or free thyroxine was also recorded if tested. Patients were included in our case series if they met the following inclusion criteria: TSH level > 100 μU/mL and same-day sodium and creatinine levels. All laboratory tests were collected on an outpatient basis.ResultsThe 10 subjects (2 men and 8 women) were ages 19 to 97 years (median, 51.5 years). Median TSH was 193 μU/mL (range, 104.2 to 515.6 μU/mL; normal, 0.40 to 5.50 μU/mL) with median sodium of 138 mmol/L (range, 136 to 142 mmol/L; normal, 135 to 146 mmol/L). The lowest sodium was 136 mmol/L with concurrent TSH of 469.7 μU/mL, free triiodothyronine of 1.0 pg/mL (normal, 1.8 to 4.6 pg/mL), and free thyroxine of 0.2 ng/ dL (normal, 0.7 to 1.8 ng/dL). Median GFR was 67.5 mL/ min/1.73 m2 (range, 44 to 114 mL/min/1.73 m2; normal, 90 to 120 mL/min/1.73 m2).ConclusionIn our small series of patients with extreme TSH elevations, none had a serum sodium level below normal (< 135 mmol/L), even in the presence of a reduced GFR. Hyponatremia can be a common occurrence in hospitalized and/or chronically ill patients; however, in an otherwise relatively healthy ambulatory patient, hypothyroidism, even when severely undertreated, may be a less clinically relevant cause of hyponatremia. (Endocr Pract. 2012;18:894-897)  相似文献   

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In this study, we evaluated, for the first time, the application of molecular tube based alpha-cyclodextrin for improving the refolding yields of two different enzymes: carbonic anhydrase and alkaline phosphatase. Our results indicate that under the optimal developed refolding environments, the denatured carbonic anhydrase and alkaline phosphatase were refolded with a yield of 51 and 61% using 15 and 5 mg/ml of the molecular tube, respectively. Regardless of lower refolding yields compared with liquid-phase artificial chaperone assisted approach, the new technique (solid-phase artificial chaperone assisted refolding) benefits from easier and faster separation of the refolded product from the refolding environment, recycling of the stripping agent, and finally, significantly less environmental effect at the industrial levels. However, further improvements in solid-phase artificial chaperone assisted technique are needed either through synthesizing better stripping agents or by optimizing and defining better refolding environments.  相似文献   

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Fibrosis is characterized by excessive accumulation of collagen and other extracellular matrix (ECM) components, and this process has been likened to aberrant wound healing. The early phases of wound healing involve the formation of a provisional ECM containing fibrin, fibrinogen, and fibronectin. Fibroblasts occupy this matrix and proliferate in response to activators elaborated by leukocytes that have migrated into the wound and are retained by the ECM. This coincides with the appearance of the myofibroblast, a specialized form of fibroblast whose differentiation is primarily driven by cytokines, such as transforming growth factor-β (TGF-β), and by mechanical tension. When these signals are reduced, as when TGF-β secretion is reduced, or as in scar shrinkage, myofibroblasts undergo apoptosis, resulting in a collagen-rich, cell-poor scar. Retention of myofibroblasts in fibrosis has been described as the result of imbalanced cytokine signaling, especially with respect to levels of activated TGF-β. ECM components can regulate myofibroblast persistence directly, since this phenotype is dependent on extracellular hyaluronan, tenascin-C, and the fibronectin splice variant containing the "extra domain A," and also, indirectly, through retention of TGF-β-secreting cells such as eosinophils. Thus the ECM is actively involved in both cellular and extracellular events that lead to fibrosis. Targeting components of the ECM as cells respond to injury and inflammatory stimuli holds promise as a means to avoid development of fibrosis and direct the wound-healing process toward reestablishment of a healthy equilibrium.  相似文献   

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Four previously much confused species of Lecythis, which form a coherent group of species collectively known in Brazil as “sapucaias,” are described and differentiated in a key. A summary of their pollination and dispersal is presented as well as of their present-day distributions in relation to past geological and climatological events. Fruit variability, the cause of name proliferation in this group, is described and related to the problem of species concepts in the Lecythidaceae.  相似文献   

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