Seminum 2018
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UPDATED 18Th February 2013
7th February 2015 Welcome to my new seed trade list for 2014-15. 12, 13 and 14 in brackets indicates the harvesting year for the seed. Concerning seed quantity: as I don't have many plants of each species, seed quantity is limited in most cases. Therefore, for some species you may only get a few seeds. Many species are harvested in my garden. Others are surplus from trade and purchase. OUT: Means out of stock. Sometimes I sell surplus seed (if time allows), although this is unlikely this season. NB! Cultivars do not always come true. I offer them anyway, but no guarantees to what you will get! Botanical Name (year of harvest) NB! Traditional vegetables are at the end of the list with (mostly) common English names first. Acanthopanax henryi (14) Achillea sibirica (13) Aconitum lamarckii (12) Achyranthes aspera (14, 13) Adenophora khasiana (13) Adenophora triphylla (13) Agastache anisata (14,13)N Agastache anisata alba (13)N Agastache rugosa (Ex-Japan) (13) (two varieties) Agrostemma githago (13)1 Alcea rosea “Nigra” (13) Allium albidum (13) Allium altissimum (Persian Shallot) (14) Allium atroviolaceum (13) Allium beesianum (14,12) Allium brevistylum (14) Allium caeruleum (14)E Allium carinatum ssp. pulchellum (14) Allium carinatum ssp. pulchellum album (14)E Allium carolinianum (13)N Allium cernuum mix (14) E/N Allium cernuum “Dark Scape” (14)E Allium cernuum ‘Dwarf White” (14)E Allium cernuum ‘Pink Giant’ (14)N Allium cernuum x stellatum (14)E (received as cernuum , but it looks like a hybrid with stellatum, from SSE, OR KA A) Allium cernuum x stellatum (14)E (received as cernuum from a local garden centre) Allium clathratum (13) Allium crenulatum (13) Wild coll. -
Geological Excursion BASE-Line Earth
Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17 -
Zur Geologie Des Hochlantsch (Grazer Paläozoikum, Steiermark)
Jb. Geol. B.-A. ISSN 0016-7800 Band 128 S.43-73 Wien, Mai 1985 Zur Geologie des Hochlantsch (Grazer Paläozoikum, Steiermark) Von JOHANN GOLLNER & CHRISTIAN ZIER*) Mit 9 Abbildungen, 2 Tabellen und 6 Tafeln Steiermark Grazer Paläozoikum Stratigraphie 6sterreichische Karte1: 50.000 Fazies Blatt 134 Tektonik Inhalt Zusammenfassung, Summary 43 1. 6i;~e~~~~O~~ik~~':::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::: 1.1. Die Hochlantschgruppe 44 1.1.1. Dolomitsandsteinfolge 46 1.1.2. "Gesteine des Breitalmkreuz" 47 1.1.3. Barrandeischichten " 47 1.1.4. Tyrnauer Alm-Formation 48 1.1.5. Zachenspitzformation 50 1.1.6. Steinbergkalk 51 1.1.7. Hochlantschkalk 51 1.1.8. Mixnitzer Karbon 52 1.2. Laufnitzdorfer Gruppe 52 1.3. "Kalkschieferfolge" 53 1.3.1. Tektonische Position der "Kalkschieferfolge" 53 1.3:2. "Gschwendtformation", "Heubergformation" , "Koglerformation", "Höllgrabeneinheit" 53 1.3.3. Größkogelgruppe 54 2. Postpaläozoische Ablagerungen 55 2.1. Gams/Bärenschützkonglomerat 55 2.2. Tertiärkonglomerat 55 2.3. Burgstallbrekzie 55 2.4. Gehängebrekzien und Schuttbildungen 56 2.5. Quartäre Spalten 57 3. Tektonischer Bau 57 ~i~;r~tu'r' : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : ~g Zusammenfassung campan) verglichen wird, tritt in unterschiedlichen Höhenni- Der Hochlantsch als nördlicher Eckpfeiler des Grazer Paläo- veaus im Hangenden des Hochlantschkalks (Hochlantschgrup- zoikums ist -
Seminum 2017 Tisk
FRONT COVER: Campanula cochleariifolia Lam. SK-0-PLZEN-4260-98-20 (No. 75) Slovakia, Nízké Tatry Mts., Demänovská dolina, near hotel Repiská, calcareous rocks Photo: Jaroslav Vogeltanz INDEX SEMINUM 2017 PLZE Ň 2017 1 ZOOLOGICAL AND BOTANICAL GARDEN OF THE CITY PLZEN Pod Vinicemi 9, 301 00 Plzen Czech Republic Telephone: +420/378038301 Fax: +420/378038302 E-mail: [email protected] Area: 21,5 ha Geographical location: Latitude: 49 o 44’ N Longitude: 13 o23’ E Altitude: 330 m Annual average temperature: 7,4 oC Highest annual temperature: 40 o C Lowest annual temperature: - 27 oC Annual rainfall: 512 mm Director: Ing. Ji ří Trávní ček Curator of Botany: Ing. Tomáš Peš Seed collectors: Mgr. Václava Pešková, Radka Matulová, Petra Vonášková, Lenka Richterová, Hana Janouškovcová 2 Please notice: Complying with article 15 of the Convention on Biological Diversity (CBD, 1992), the Zoological and Botanical Garden of Plzen provides seeds and any other plant material only for botanical gardens and other scientific institutions using this materiál according to the CBD. We are part of the IPEN network (International Plant Exchange Network) and can exchange material with other IPEN-members without further bi-lateral agreements.For a list of gardens currently registered with IPEN and for additional information, please refer to the BGCI website. Non IPEN-members have to return the Agreement on the supply of living plant material for non-commercial purposes leaving the International Plant Exchange Network , which must be signed by authorized staff. The IPEN number given with the seed material consists of four elements: 1. The first two characters are the international iso 3166-1-alpha-2-code of the country of origin ("XX" for unknown origin) 2. -
Seedling Establishment, Bud Movement, and Subterranean Diversity of Geophilous Systems in Apiaceae
Flora (2002) 197, 385–393 http://www.urbanfischer.de/journals/flora Seedling establishment, bud movement, and subterranean diversity of geophilous systems in Apiaceae Norbert Pütz1* & Ina Sukkau2 1 Institute of Nature Conservation and Environmental Education, University of Vechta, Driverstr. 22, D-49377 Vechta, Germany 2 Institute of Botany, RWTH Aachen, Germany * author for correspondence: e-mail: [email protected] Received: Nov 29, 2001 · Accepted: Jun 10, 2002 Summary Geophilous systems of plants are not only regarded as organs of underground storage. Such systems also undergo a large range of modifications in order to fulfill other ‚cryptical‘ functions, e.g. positioning of innovation buds, vegetative cloning, and vege- tative dispersal. Seedlings should always be the point of departure for any investigation into the structure of geophilous systems. This is because in the ability to survive of geophilous plants it is of primary importance that innovation buds can reach a safe position in the soil by the time the first period hostile to vegetation commences. Our analysis of such systems thus focused on examining the development of 34 species of the Apiaceae, beginning with their germination. Independent of life-form and life-span, all species exhibit noticeable terminal bud movement with the aid of contractile organs. Movement was found to be at least 5 mm, reaching a maximum of 45 mm. All species exhibit a noticeable contraction of the primary root. In most cases the contraction phenomenon also occurs in the hypocotyl, and some species show contraction of their lateral and / or adventitious roots. Analysis of movement shows the functional importance of pulling the inno- vation buds down into the soil. -
Show Activity
A Cytochrome-P450-Inhibitor *Unless otherwise noted all references are to Duke, James A. 1992. Handbook of phytochemical constituents of GRAS herbs and other economic plants. Boca Raton, FL. CRC Press. Plant # Chemicals Total PPM Acacia farnesiana Huisache; Cassie; Popinac; Sweet Acacia; Opopanax 2 Achillea millefolium Yarrow; Milfoil 1 Acorus calamus Flagroot; Sweetroot; Sweet Calamus; Myrtle Flag; Calamus; Sweetflag 1 384.0 Agastache rugosa 1 Ageratum conyzoides Mexican ageratum 1 Aloysia citrodora Lemon Verbena 1 Alpinia officinarum Lesser Galangal; Chinese Ginger 1 800.0 Alpinia galanga Siamese Ginger; Languas; Greater Galangal 1 24000.0 Ammi majus Bishop's Weed 2 16000.0 Anacardium occidentale Cashew 1 Anethum graveolens Garden Dill; Dill 1 Angelica dahurica Bai Zhi 2 Angelica archangelica Angelica; Wild Parsnip; Garden Angelica 2 5050.0 Apium graveolens Celery 3 Artemisia dracunculus Tarragon 2 141.0 Boronia megastigma Scented Boronia 1 Calamintha nepeta Turkish Calamint 1 Camellia sinensis Tea 2 Cananga odorata Cananga; Ylang-Ylang 1 Capsicum frutescens Tabasco; Cayenne; Chili; Hot Pepper; Spur Pepper; Red Chili 1 35800.0 Capsicum annuum Cherry Pepper; Cone Pepper; Paprika; Bell Pepper; Sweet Pepper; Green Pepper 2 8000.0 Centaurea calcitrapa Star-Thistle 1 Chenopodium album Lambsquarter 1 Cinnamomum verum Ceylon Cinnamon; Cinnamon 1 20320.0 Cinnamomum camphora Camphor; Ho Leaf 1 Cinnamomum aromaticum Cassia Lignea; Chinese Cassia; Chinesischer Zimtbaum (Ger.); Canela de la China (Sp.); 1 Saigon Cinnamon; Chinazimt (Ger.); Kashia-Keihi -
Peucedanum Ostruthium Inhibits E-Selectin and VCAM-1 Expression in Endothelial Cells Through Interference with NF-Κb Signaling
biomolecules Article Peucedanum ostruthium Inhibits E-Selectin and VCAM-1 Expression in Endothelial Cells through Interference with NF-κB Signaling Christoph Lammel 1, Julia Zwirchmayr 2 , Jaqueline Seigner 1 , Judith M. Rollinger 2,* and Rainer de Martin 1 1 Department of Vascular Biology and Thrombosis Research, Medical University of Vienna, Schwarzspanierstaße 17, 1090 Vienna, Austria; [email protected] (C.L.); [email protected] (J.S.); [email protected] (R.d.M.) 2 Department of Pharmacognosy, Faculty of Life Sciences, University of Vienna, Althanstraße 14, 1090 Vienna, Austria; [email protected] * Correspondence: [email protected]; Tel.: +43-1-4277-55255; Fax: +43-1-4277-855255 Received: 5 June 2020; Accepted: 18 August 2020; Published: 21 August 2020 Abstract: Twenty natural remedies traditionally used against different inflammatory diseases were probed for their potential to suppress the expression of the inflammatory markers E-selectin and VCAM-1 in a model system of IL-1 stimulated human umbilical vein endothelial cells (HUVEC). One third of the tested extracts showed in vitro inhibitory effects comparable to the positive control oxozeaenol, an inhibitor of TAK1. Among them, the extract derived from the roots and rhizomes of Peucedanum ostruthium (i.e., Radix Imperatoriae), also known as masterwort, showed a pronounced and dose-dependent inhibitory effect. Reporter gene analysis demonstrated that inhibition takes place on the transcriptional level and involves the transcription factor NF-κB. A more detailed analysis revealed that the P. ostruthium extract (PO) affected the phosphorylation, degradation, and resynthesis of IκBα, the activation of IKKs, and the nuclear translocation of the NF-κB subunit RelA. -
Ecology of the Olearia Colensoi Dominated Sub-Alpine Scrub in the Southern Ruahine Range, New Zealand
Copyright is owned by the Author of the thesis. Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the permission of the Author. 581 .509 9355 Ess ECOLOGY OF THE OLEARIA COLENSOI DOMINATED SUB-ALPINE SCRUB IN THE SOUTHERN RUAHINE RANGE, NEW ZEALAND. A thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Botany at Massey University New Zealand Peter Ronald van Essen 1992 Olearia colensoi in flower. Reproduced from a lithograph by Walter Fitch in Flora Novae-Zelandiae (J.D. Hooker 1852). Source: Alexander Turnbull Library in New Zealand Heritage, Paul Hamlyn Ltd ABSTRACT The Olearia colensoi (leatherwood or tupari) dominated southern Ruahine sub-alpine scrub is the largest continuous area of sub-alpine asteraceous scrub in New Zealand - the result of a lowered treeline due to climatic conditions characterised by high cloud cover, high rainfall, and high winds and the absence of high altitude Nothofagus species. Meteorological investigation of seven sites in the southern Ruahine found that altitude alone was the main environmental detenninant of climatic variation, particularly temperature regime. Temperatures varied between sites at a lapse rate of 0.61°C lOOm-1 while daily fluctuation patterns were uniform for all sites. Rainfall increased with altitude over the Range-at a rate of 3.8mm m-1. Cloud interception, unrecorded by standard rain gauges, adds significantly to total 'rainfall'. Vegetative phenology of Olearia colensoi is highly seasonal and regular with an annual growth flush from mid November to January. -
Young Uplift in the Non-Glaciated Parts of the Eastern Alps, Earth Planet
THOMAS WAGNER YOUNG UPLIFT IN THE NON -GLACIATED PARTS OF THE EASTERN ALPS GEOMORPHOLOGICAL AND GEOCHRONOLOGICAL CONSTRAINTS A dissertation submitted to the Faculty of Natural Science Karl-Franzens University of Graz Austria for the Degree of Doctor of Science September 2010 “Only those who will risk going too far can possibly find out how far one can go.” T.S. Eliot PREAMBLE The study of the growth of mountains and the evolution of their landforms is a subject at the heart of Earth sciences. However, only newly available geochronological methods allow to constrain the timing of formation of landforms in more detail. In particular the evolution of landforms in Pliocene to Pleistocene times is much debated, because of a worldwide increase in sedimentation rates observed at the same time. Climate changes and tectonic processes are possible candidates to explain this increase. The research effort presented in this thesis fills the gap of knowledge concerning the topographic evolution of the last few million years to today’s face of a region along the eastern margin of the Alps: the Styrian Block. This block includes the Styrian Basin and its surrounding basement. New time constraints from various cave, stream and fault deposits are reported and are interpreted in terms of river incision rates, aggradation and re-excavation events. Uplift rates of the region are estimated. DEM data are used to identify the geomorphic disequilibrium of the whole Alps. The results support the notion that tectonically driven deformation and responding erosion is taking place to an increased level over the last 5-6 Ma. -
Pixel- Vs. Object-Based Landsat 8 Data Classification in Google Earth
remote sensing Article Pixel- vs. Object-Based Landsat 8 Data Classification in Google Earth Engine Using Random Forest: The Case Study of Maiella National Park Andrea Tassi 1, Daniela Gigante 1, Giuseppe Modica 2 , Luciano Di Martino 3 and Marco Vizzari 1,* 1 Department of Agricultural, Food, and Environmental Sciences, University of Perugia, 06121 Perugia, Italy; [email protected] (A.T.); [email protected] (D.G.) 2 Dipartimento di Agraria, Università degli Studi Mediterranea di Reggio Calabria, Località Feo di Vito, 89122 Reggio Calabria, Italy; [email protected] 3 Maiella National Park, Via Badia 28, 67039 Sulmona, Italy; [email protected] * Correspondence: [email protected]; Tel.: +39-075-585-6059 Abstract: With the general objective of producing a 2018–2020 Land Use/Land Cover (LULC) map of the Maiella National Park (central Italy), useful for a future long-term LULC change analysis, this research aimed to develop a Landsat 8 (L8) data composition and classification process using Google Earth Engine (GEE). In this process, we compared two pixel-based (PB) and two object-based (OB) approaches, assessing the advantages of integrating the textural information in the PB approach. Moreover, we tested the possibility of using the L8 panchromatic band to improve the segmentation step and the object’s textural analysis of the OB approach and produce a 15-m resolution LULC map. After selecting the best time window of the year to compose the base data cube, we applied a cloud-filtering and a topography-correction process on the 32 available L8 surface reflectance images. Citation: Tassi, A.; Gigante, D.; On this basis, we calculated five spectral indices, some of them on an interannual basis, to account Modica, G.; Di Martino, L.; Vizzari, M. -
L'italia Geografica
L’ITALIA GEOGRAFICA 1. L’Italia e il suo territorio Il territorio italiano è prevalentemente montuoso e collinare. Solo il 23% è occupato da zone pianeggianti. La Pianura Padana è la più estesa di tutte. Le altre occupano una superficie minore e sono localizzate sulle coste o lungo il corso dei fiumi. I fiumi Ci sono fiumi alpini e fiummi appeninici. I fiumi alpini sono alimentati dalle piogge, dalle nevi e dai ghiacciai e sono generalmente i più lunghi e ricchi d’acqua. Il più lungo è il fiume Po, che nasce dal Monviso, in Piemonte, attraversa da ovest a est tutta la Pianura Padana e si getta nel mare Adriatico. Il Po ha numerosi affluenti che scendono sia dalla Alpi, affluenti di sinistra, sia dall’Appennino, affluenti di destra. I laghi Il lago più grande d’Italia è il lago di Garda che si trova ai piedi delle Alpi. I maggiori laghi italiani, di origine glaciale, si trovano ai piedi delle Alpi e sono il lago Maggiore, il lago di Como, il lago d’Iseo. Nell’Italia centrale si trovano il lago Trasimeno, il lago di Bolsena e il lago di Bracciano. Le montagne Le Alpi, che dividono la penisola italiana dal resto d’Europa, si estendono per circa 1200 da est a ovest. Ricche di ghiacciai, danno origine a numerosi fiumi. La cima più alta è il Monte Bianco (4810m, in Valle d’Aosta) che è anche la più alta d’Europa. Seguono il Monte Rosa (Piemonte), il Cervino (Piemonte) e il Gran Paradiso (tra Val d’Aosta e Piemonte). -
Rivista Mensile Del Centro Alpinistico Italiano N.1-2-3
RIVISTA MENSILE DEL CENTRO ALPINISTICO ITALIANO N.1-2-3 oma av. - te. ennalo SPEDIZIONE IN ABBONAMENTO POSTALE A MILANO - GRUPPO 'A' COPIE 50.0 C) O Direttore i ANGELO MANARESI Direzione, Amministrazione, Comitato delle pubblicazioni: ROMA Corso Umberto, 4 - Telef. 67-446 Ufficio Pubblicità in Milano, Via Moacova N. 18 Telefono 66-793 Gratis ai soci del C.A.I. La collaborazione viene retribuita - Manoscritti e illustrazioni non vengono restituiti in nessun caso SOMMARIO In coperima Sul Lago di Scanno. in Abruz- Cinema in montagna, (con r tavola fuori testo) - zo. neg. C. Landi Vittori. S. Ten. Alfonso Vinci. Soci del C.A.I. caduti in guerra. Il Trofeo della Montagna del C.A.I. nuo- Soci del C.A.I. decorati al Valor Militare. vamente assegnato alla G.I.L. di Aosta Antelao. m. 3263, (con i tavola fuori testo) - Pie- Un prezioso esemplare della flora alpina ralberto Sagramora. a servizio dell'autarchia del farmaco Con De Saussure attorno al Monte Rosa. in Italia - Prof Piero Mascherpa. (con i djsegno e i tavola fuori testo! - Dr. Silvio Saglio. Monte Rotella. m. 2127. (con i disegno e ta » fuori testo) - Ing. Carlo Landi Vittorr. Prime ascensioni invernali nel Gruppo Gianfranco Campestrini pittore di mon- 2 tavole del Gran Paradiso, (con i disegno e tagna, (con i tavola fuori testo) - Emilio Bernasconi. fuori testo) - Prof. Leopoldo Saletti - Don Pietro Solero. Cronaca alpina (con i tavola fuori testo) Primati alpinistici - Doti Ettore Castiglioni. NOTI ZI ARIO • Della sonda per valanghe. (con I disegno) - Soci caduti in guerra - Atti e Comunicati della Presidenza Gianni Marini.