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31 results for “Mediterranean flora”
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils. in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils.
Text-fig. 1. Modern vegetation proxies as delivered by the Drudge 1 and 2 tools for Parschlug. Left column results from KovarEder et al. (2021) based on the floristic spectrum published by Kovar-Eder et al. (2004). The other three columns result from three variants using the enlarged floristic spectrum herein. Differences between variants 1–3 from this study are caused by differences in assignment of some taxa and morphotypes (see Appendix 1). European vegetation formations: Formation C – Subarctic, boreal and nemoral-montane open woodlands as well as subalpine and oro-Mediterranean vegetation; Formation D – Mesophytic and hygromesophytic coniferous and mixed broad-leaved-coniferous forests; Formation F – Mesophytic broadleaved deciduous and mixed broadleaved/conifer forests; Formation G – Thermophilous mixed deciduous broadleaved forests; Formation J – Mediterranean sclerophyllous forests and scrub; Formation K – Xerophytic coniferous forests, coniferous woodland and scrub. East Asian vegetation types: MCF China, Japan – Montane Coniferous Forests China, Honshu, Yakushima; BLDF N and NE Provinces, China – Broad-leaved Deciduous Forests of the Northern and Northeastern Provinces (China); BLDF Upper Yangtze, Honshu – Broad-leaved Deciduous Forest, Upper Yangtze Provinces, Mt. Emei, and Honshu; MMF China – Mixed Mesophytic Forest, Lower Yangtze Provinces; BLEF China, Japan – Broad-leaved Evergreen Forests, China, Japan; Meili Snow Mt. high altitude SCL and BLF, China – Meili Snow Mt., Sclerophyllous and broad-leaved forest zone (2,580-3,650 m alt.). (Designations of European vegetation formations follow Bohn et al. (2004) and Asian ones follow Kovar-Eder et al. (2021). in Floristic, Vegetation And Climate Assessment Of The Early/Middle Miocene Parschlug Flora Indicates A Distinctly Seasonal Climate
Text-fig. 1. Modern vegetation proxies as delivered by the Drudge 1 and 2 tools for Parschlug. Left column results from KovarEder et al. (2021) based on the floristic spectrum published by Kovar-Eder et al. (2004). The other three columns result from three variants using the enlarged floristic spectrum herein. Differences between variants 1–3 from this study are caused by differences in assignment of some taxa and morphotypes (see Appendix 1). European vegetation formations: Formation C – Subarctic, boreal and nemoral-montane open woodlands as well as subalpine and oro-Mediterranean vegetation; Formation D – Mesophytic and hygromesophytic coniferous and mixed broad-leaved-coniferous forests; Formation F – Mesophytic broadleaved deciduous and mixed broadleaved/conifer forests; Formation G – Thermophilous mixed deciduous broadleaved forests; Formation J – Mediterranean sclerophyllous forests and scrub; Formation K – Xerophytic coniferous forests, coniferous woodland and scrub. East Asian vegetation types: MCF China, Japan – Montane Coniferous Forests China, Honshu, Yakushima; BLDF N and NE Provinces, China – Broad-leaved Deciduous Forests of the Northern and Northeastern Provinces (China); BLDF Upper Yangtze, Honshu – Broad-leaved Deciduous Forest, Upper Yangtze Provinces, Mt. Emei, and Honshu; MMF China – Mixed Mesophytic Forest, Lower Yangtze Provinces; BLEF China, Japan – Broad-leaved Evergreen Forests, China, Japan; Meili Snow Mt. high altitude SCL and BLF, China – Meili Snow Mt., Sclerophyllous and broad-leaved forest zone (2,580-3,650 m alt.). (Designations of European vegetation formations follow Bohn et al. (2004) and Asian ones follow Kovar-Eder et al. (2021).
Fig. 2 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 2 - Geographical distribution in Sicily of Vitis labrusca (green dots), V. ×instabilis (red dots), and V. ×koberi (blue dots).
Fig. 5 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 5 - Rootstocks of Vitis ×ruggerii '140 Ru' emerging from an abandoned vineyard in �cate (Photo: N.M.G. �rdenghi).
Fig. 1 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 1 - Geographical distribution in Sicily of Vitis rupestris (red dots), Vitis ×goliath (green dots), and Vitis ×ruggerii (blue dots).
Fig. 4 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 4 - Invasive stand of Vitis ×ruggerii '775 P' in �cate, with the first author posing for scale. The plant completely covers the fence of an olive grove and, on the extreme right, an almond tree (Photo: P. Cauzzi).
Fig. 3 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 3 - Vitis ×koberi in Sutera: a) invasive stand along the railway; b) leaf blades (Photos: N.M.G. Ardenghi).
Fig. 7 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 7 - Vitis rupestris: a) invasive monospecific stand in Mezzojuso; b) leaf blades (Photos: N.M.G. �rdenghi).
Fig. 6 in Alien grapes (Vitis, Vitaceae) in Sicily (Italy): novelties for the Sicilian and Mediterranean flora
Fig. 6 - Vitis ×ruggerii: a) typical entire leaf blades; b-c) cultivar '57 R' with lobed leaf blades (Photos: N. M. G. �rdenghi).
Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011). in Feather Palm Foliage From The Messinian Of Italy (Capo Di Fiume, Palena And Pollenzo Near Alba) Within The Framework Of Northern Mediterranean Late Miocene Flora
Text-fig. 1. A. Location of the sites of Capo di Fiume, Palena and Pollenzo near Alba. B. Capo di Fiume stratigraphic section. Facies of coastal-transitional marine associations – a. Freshwater marsh and tidal creeks interval, b. Swamp interval, c1–c4. Facies of eustarine bay associations, d1–d6. Facies of open shelf marine associations. Symbols: "black star" – fossiliferous horizon with plant material studied here, 1. mottled grey to dark-brown marls and clayey marls, 2. fissile dark-grey marls and shaly marls, 3. limestones, 4. marly limestones and limey marls, 5. bio-lithoclastic calcarenites, 6. lime conglomerate, 7. massive muddy deposit produced by mass-flow mechanism, 8. diatomitic marls, 9. "terra rossa" soil (modified after Carnevale et al. 2011).
Genus level DNA sequence data for three genes (matK, rbcL, trnH-psbA) for the paper: A comprehensive, genus-level time-calibrated phylogeny of the tree flora of Mediterranean Europe and an assessment of its vulnerability
<p>This data file contains the consensus DNA sequences in fasta format, of 64 tree genera found in Mediterranean Europe, following the checklist of Médail et al. (2019). </p> <p>The data are used in a manuscript submitted for publication to Botany Letters and currently under revision. The manuscript is entitled: "<em>A comprehensive, genus-level time-calibrated phylogeny of the tree flora of Mediterranean Europe and an assessment of its vulnerability</em>". Its authors are: Marwan Cheikh Albassatneh, Marcial Escudero, Loic Ponge<sup>*</sup>, Anne-Christine Monnet, Juan Arroyo, Toni Nikolic, Gianluigi Bacchetta, Francesca Bagnoli, Panayotis Dimopoulos, Agathe Leriche, Frédéric Médail, Anne Roig, Ilaria Spanu, Giovanni Giuseppe Vendramin, Arndt Hampe, Bruno Fady.</p>
Data from: Phenological patterns in Mediterranean south Iberian serpentine flora
Phenological phases, as adaptive strategies, have been studied in Mediterranean serpentine shrubland vegetation and their endemisms, in the South of the Iberian Peninsula. The aim of this research is to obtain the phenological characterization of the serpentine flora and to make a comparison between endemic serpentine and non‐serpentine plants in different years and altitudes. For this purpose, data were taken in the serpentine ecosystem of Sierra Bermeja (Andalusia, Spain) establishing two plots on two altitudinal bioclimatic belts and during two different years. A total of 28 persistent taxa were studied, focusing on serpentinophytes, their allied (magnesicolous) and non‐serpentinophytes, trying to detect the possible differences between serpentine endemic taxa and non‐endemic plants. Phenological calendars and phenological patterns (phenophasic indexes) were obtained. The species showed phenophasic patterns similar to those of other studied Mediterranean flora: a phenological pause which coincides with summer and most plants behaved as summer semi‐deciduous with seasonal dimorphism. There were no statistically significant differences in phenology and in phenological indexes due to the altitude, to the year of sampling and due to the serpentine affinity. The best represented active phenophasic period of the species was 9‐11 months of activity although showing the summer phenological pause. Species with low index of reproductive/vegetative activity of the species predominated, employing more time/resources for vegetative functions, and with synchronous phenophases, where flowering and growth coincide (phenophasic pattern type I). The phenophasic period of serpentinophytes and magnesicolous taxa pointed to a certain delay in the period of flowering with respect to the group of non‐serpentinophytes, a result which could have reproductive implications.
FIGURE 8 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 8. Phenological features of Bituminaria palaestina A. Natural habitat with Platanus orientalis in Ajloun (Jordan). B and C. Detail of flowering stems. D. Detail of leaves. E and F. detail of inflorescence (Photos by G. Giusso del Galdo).
FIGURE 6 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 6. SEM micrographs of pollen grains of Bituminaria bituminosa (A) from Catania (Sicily) and B. palaestina (B) from Hula Valley (Israel), at low magnification (1–2 × 1600) and at high magnification (3 × 4000). (A: Catania, S. Brullo s.n., CAT; B: Hula Valley, S. Brullo s.n., CAT).
FIGURE 2 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 2. Diagnostic features regarding the vegetative structures of Bituminaria palaestina. A. Habit. B. Leaves. C. Leaf apex (abaxial side). D. Leaf apex (adaxial side). E. Stipules. Illustration by S. Brullo based on living material coming from Hula Valley in Israel (S. Brullo s.n., CAT).
FIGURE 5 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 5. SEM micrographs of seed testa (A1–3, B1–3) and pod hairs (B4–5) of Bituminaria palaestina from Hula Valley in Israel (A1–3) and from Ajloun in Jordan (B1–5) at low magnification (A1 and B1 × 15), at medium magnification (B4 × 250; B5 × 700; A2 and B2 × 1000), and at high magnification (A3 and B3 × 2500) from material cultivated at the Botanical Garden of Catania (A: Hula Valley, S. Brullo s.n., CAT; B: Ajloun, Giusso, Minissale & Ananbeh s.n. CAT).
FIGURE 4 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 4. Two mitotic metaphase plates (2n = 20) of Bituminaria palaestina from Hula Valley (Israel). Scale bar = 10 μm.
FIGURE 1 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 1. Illustration of Psoralea palaestina published by Bassi (1768, Tab.2), lectotype of this species.
FIGURE 3 in Taxonomic investigations on Psoralea palaestina (Fabaceae), a critical species of Mediterranean flora
FIGURE 3. Diagnostic features regarding the reproductive structures of Bituminaria palaestina A. Flower (ventral view). B. Flower (dorsal view). C. Flower (lateral view). D. Bud. E. Calyx (open). F. Standars. G. Wings. H. Keel (open). I. Keel (lateral view). J. Staminal tube. K. Anther. L. Pistil. M. Stigma. N. Fruiting calyx and pod. O. Pods. P. Seed. Illustration by S. Brullo based on living material coming from Hula Valley in Israel (S. Brullo s.n., CAT).
FIGURE 4 in Why so different? A case study about Floras from a Mediterranean island
FIGURE 4. Repartition in different categories of the 298 taxa considered as P in ARR and in different way in BAR. P=Occurring; D=Doubtfully occurring or no longer recorded; NP=Recorded by mistake; C=Cryptogenic; A=Alien.
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