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Artykuły w czasopismach na temat "Non-vascular plants"
RAVEN, J. A. "Long-distance transport in non-vascular plants". Plant, Cell & Environment 26, nr 1 (styczeń 2003): 73–85. http://dx.doi.org/10.1046/j.1365-3040.2003.00920.x.
Pełny tekst źródłaSchneider-Poetsch, Hansjörg A. W., Üner Kolukisaoglu, David H. Clapham, Jon Hughes i Tilman Lamparter. "Non-angiosperm phytochromes and the evolution of vascular plants". Physiologia Plantarum 102, nr 4 (kwiecień 1998): 612–22. http://dx.doi.org/10.1034/j.1399-3054.1998.1020417.x.
Pełny tekst źródłaEldridge, David John. "Conservation of non-vascular plants in semi-arid conditions". Danthonia: newsletter of the Australian Network for Plant Conservation 8, nr 1 (czerwiec 1999): 1. http://dx.doi.org/10.5962/p.374085.
Pełny tekst źródłaNicol, Lauren, Wojciech J. Nawrocki i Roberta Croce. "Disentangling the sites of non-photochemical quenching in vascular plants". Nature Plants 5, nr 11 (28.10.2019): 1177–83. http://dx.doi.org/10.1038/s41477-019-0526-5.
Pełny tekst źródłaSato, Naoki, i Masaki Furuya. "Distribution of diacylglyceryltrimethylhomoserine and phosphatidylcholine in non-vascular green plants". Plant Science 38, nr 2 (marzec 1985): 81–85. http://dx.doi.org/10.1016/0168-9452(85)90134-7.
Pełny tekst źródłaCameron, Robert. "Red Maple, Acer rubrum, Wetland Composition and Structure in Nova Scotia". Canadian Field-Naturalist 123, nr 3 (1.07.2009): 221. http://dx.doi.org/10.22621/cfn.v123i3.968.
Pełny tekst źródłaHnatowich, Ian G., Eric G. Lamb i Katherine J. Stewart. "Reintroducing Vascular and Non-Vascular Plants to Disturbed Arctic Sites: Investigating Turfs and Turf Fragments". Ecological Restoration 41, nr 1 (marzec 2023): 3–15. http://dx.doi.org/10.3368/er.41.1.3.
Pełny tekst źródłaVerloove, Filip, i Nicola Ardenghi. "New distributional records of non-native vascular plants in northern Italy". Natural History Sciences 2, nr 1 (30.06.2015): 5. http://dx.doi.org/10.4081/nhs.2015.219.
Pełny tekst źródłaKnoll, A. H., S. W. F. Grant i J. W. Tsao. "The Early Evolution of Land Plants". Notes for a Short Course: Studies in Geology 15 (1986): 45–63. http://dx.doi.org/10.1017/s0271164800001329.
Pełny tekst źródłaRosenstiel, Todd N., i Sarah M. Eppley. "Long-lived sperm in the geothermal bryophyte Pohlia nutans". Biology Letters 5, nr 6 (29.07.2009): 857–60. http://dx.doi.org/10.1098/rsbl.2009.0380.
Pełny tekst źródłaRozprawy doktorskie na temat "Non-vascular plants"
Kowal, Jill. "Fungal interactions with vascular and non-vascular plants : an investigation of mutualisms and their roles in heathland regeneration". Thesis, Imperial College London, 2016. http://hdl.handle.net/10044/1/42788.
Pełny tekst źródłaPohl, Alexandre. "Compréhension du climat de l’Ordovicien à l’aide de la modélisation numérique". Thesis, Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLV081.
Pełny tekst źródłaThe Ordovician (485–444 Ma) is a geological period characterized by theconcomitance of a major glaciation and one of the “Big Five” mass extinction events thatpunctuated the Earth’s history. This dissertation aimed at developing a better understandingof the climatic evolution at that time through numerical modeling, in order to providea consistent picture of the glaciation. First, it was shown that the Ordovician continentalconiguration leads to a particular ocean dynamics, which induces in turn the development ofa climatic instability that allows global climate to cool suddenly in response to subtle changesin the atmospheric partial pressure of CO2 (pCO2). Secondly, an innovative climate-ice sheetcoupled model produced the irst simulation of the glaciation that is supported by geologicaldata, in the context of a decrease in pCO2. Results show that glacial onset may have occurredas early as the Mid Ordovician (465 Ma), i.e., some 20 million years earlier than thoughtinitially. In this scenario, the climatic instability is reached during the latest Ordovician andaccounts for the onset of the Hirnantian glacial maximum (445–444 Ma). Experiments conductedwith a non-vascular vegetation model reveal that the origination and expansion of theirst land plants signiicantly intensiied continental weathering during the Ordovician andpotentially drove the drop in atmospheric CO2. Finally, the interactions between climate andthe marine biosphere were investigated based on 2 complementary axes. (i) News constraintson the paleobiogeography of marine living communities were brought through the publicationof maps showing the ocean surface circulation modeled at various pCO2 levels during theEarly, Middle and Late Ordovician. (ii) The relationships between climatic variations andthe redox state of the ocean were studied using a recent ocean model with biogeochemical capabilities(MITgcm). The simulations suggest partial and global oceanic anoxic events duringthe Katian and the early Silurian respectively. They also show that anoxia is probably notresponsible for the latest Ordovician mass extinction event
Pohl, Alexandre. "Compréhension du climat de l’Ordovicien à l’aide de la modélisation numérique". Electronic Thesis or Diss., Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLV081.
Pełny tekst źródłaThe Ordovician (485–444 Ma) is a geological period characterized by theconcomitance of a major glaciation and one of the “Big Five” mass extinction events thatpunctuated the Earth’s history. This dissertation aimed at developing a better understandingof the climatic evolution at that time through numerical modeling, in order to providea consistent picture of the glaciation. First, it was shown that the Ordovician continentalconiguration leads to a particular ocean dynamics, which induces in turn the development ofa climatic instability that allows global climate to cool suddenly in response to subtle changesin the atmospheric partial pressure of CO2 (pCO2). Secondly, an innovative climate-ice sheetcoupled model produced the irst simulation of the glaciation that is supported by geologicaldata, in the context of a decrease in pCO2. Results show that glacial onset may have occurredas early as the Mid Ordovician (465 Ma), i.e., some 20 million years earlier than thoughtinitially. In this scenario, the climatic instability is reached during the latest Ordovician andaccounts for the onset of the Hirnantian glacial maximum (445–444 Ma). Experiments conductedwith a non-vascular vegetation model reveal that the origination and expansion of theirst land plants signiicantly intensiied continental weathering during the Ordovician andpotentially drove the drop in atmospheric CO2. Finally, the interactions between climate andthe marine biosphere were investigated based on 2 complementary axes. (i) News constraintson the paleobiogeography of marine living communities were brought through the publicationof maps showing the ocean surface circulation modeled at various pCO2 levels during theEarly, Middle and Late Ordovician. (ii) The relationships between climatic variations andthe redox state of the ocean were studied using a recent ocean model with biogeochemical capabilities(MITgcm). The simulations suggest partial and global oceanic anoxic events duringthe Katian and the early Silurian respectively. They also show that anoxia is probably notresponsible for the latest Ordovician mass extinction event
Affeld, Kathrin. "Spatial complexity and microclimatic responses of epiphyte communities and their invertebrate fauna in the canopy of northern rata (Metrosideros robusta A. Cunn.: Myrtaceae) on the West Coast of the South Island, New Zealand". Diss., Lincoln University, 2008. http://hdl.handle.net/10182/771.
Pełny tekst źródłaMensi, Imène. "Localisation in planta de Xanthomonas albilineans et identification de déterminants moléculaires impliqués dans la colonisation épiphyte de sa plante hôte, la canne à sucre". Thesis, Montpellier 2, 2013. http://www.theses.fr/2013MON20157.
Pełny tekst źródłaXanthomonas albilineans is the causal agent of leaf scald, a lethal disease of sugarcane that can significantly impact infected susceptible varieties in the field. The mechanisms that govern the interactions between this bacterial pathogen and its host plant are not well known. The objectives of this study were (i) to identify molecular factors involved in epiphytic survival of X. albilineans and (ii) to verify the localization of X. albilineans in sugarcane tissues. Among the studied factors, surface polysaccharides and an outer-membrane protein (XaOmpA1) of X. albilineans were crucial for epiphytic survival of this pathogen. Secondary metabolites synthesized by non-ribosomal peptide synthetases and the diffusible signal factor DSF were not critical for survival of X. albilineans on the sugarcane leaf surface, at least in absence of competing microorganisms. However, an intact DSF/RpfGC system was necessary for optimal colonization of the phyllosphere. In the second part of this study, we verified in planta localization of X. albilineans by confocal microscopy, immunochemistry and transmission electron microscopy. Microscopic observations allowed us to show that X. albilineans is not a xylem limited bacterium as it was believed until now. This pathogen is able to invade numerous cellular types including vascular and non-vascular parenchyma cells. To our knowledge, this is a novel invasion strategy of a plant pathogenic bacterium that has not previously been described, and that remains to be deciphered
Caine, Robert. "Towards the identification and characterisation of toolkit genes responsible for stomatal development and CO2 response in the non-vascular land plant, Physcomitrella patens". Thesis, University of Sheffield, 2016. http://etheses.whiterose.ac.uk/16240/.
Pełny tekst źródłaMaliniemi, T. (Tuija). "Decadal time-scale vegetation changes at high latitudes:responses to climatic and non-climatic drivers". Doctoral thesis, Oulun yliopisto, 2018. http://urn.fi/urn:isbn:9789526220123.
Pełny tekst źródłaTiivistelmä Poikkeuksellisen nopea ilmastonmuutos on johtanut viime vuosikymmenten aikana muutoksiin boreaalisissa ja arktisissa kasviyhteisöissä. Muutoksiin lukeutuvat tuottavuuden lisääntyminen, levinneisyysrajojen siirtyminen sekä muutokset biodiversiteetissä, mitkä kaikki muuttavat ekosysteemien toimintaa. Kasvillisuuden dynamiikkaa säätelevät kuitenkin useat paikallistason tekijät, minkä seurauksena ei ole täysin selvää, miten kasvillisuus on eri alueilla ja habitaateissa muuttunut. Koska kasvillisuuden jatkuva monitorointi on harvinaista pohjoisilla alueilla, vanhojen kasvillisuusaineistojen uudelleenkartoituksista on tullut tärkeä menetelmä muutosten havaitsemiseksi. Tutkin väitöskirjassani vuosikymmenten kuluessa tapahtuneita (23–60 vuotta) kasvillisuusmuutoksia Pohjois-Fennoskandian metsissä, puuttomilla kankailla ja tundralla uudelleenkartoitusten ja kokeellisen tutkimuksen avulla, ja kytkin ne ilmastonmuutokseen sekä tärkeimpiin paikallisiin tekijöihin. Yleisiä trendejä uudelleenkartoitetuilla puuttomilla kankailla olivat variksenmarjan (Empetrum nigrum ssp. hermaphroditum) voimakas lisääntyminen lumensuojaisissa habitaateissa sekä jäkälien väheneminen kaikkialla. Yhteisöjen kokonaismuutos oli voimakkainta eteläisillä puuttomilla kankailla, jossa se korreloi yhtä aikaa lisääntyneiden lämpötilojen ja laidunpaineen kanssa. Kokeellinen tutkimus tundralla osoitti, että kasviyhteisöt kehittyvät hyvin erilaisiksi paikallisten tekijöiden voimakkuussuhteista riippuen, jotka voivat joko hidastaa tai nopeuttaa ympäristömuutoksista johtuvia kasvillisuusmuutoksia. Metsien uudelleenkartoitus osoitti yhteisöjen kokonaismuutoksen olevan pitkällä aikavälillä suurempaa tuottavilla maaperillä lehtometsissä verrattuna karumpiin kangasmetsiin. Tutkimuksen mukaan maaperän tuottavuus on avaintekijä, joka ennustaa kasvillisuusmuutosten voimakkuutta ilmastonmuutoksen aikana. Tästä tärkeästä löydöstä oli aiemmin pääasiassa vain kokeellista tutkimustietoa. Yleisistä trendeistä huolimatta, muutokset diversiteetissä, kasviryhmissä ja yksittäisissä lajeissa olivat kuitenkin vaihtelevia ja usein habitaatti- tai aluesidonnaisia. Väitöskirjani tulokset, jotka muodostavat myös aikasarjan tuleville tutkimuksille, osoittavat kasvillisuuden monitoroinnin ja uudelleenkartoitusten olevan ensisijaisen tärkeitä, jotta kasvillisuuden dynamiikkaa voidaan ymmärtää paremmin nopeasti muuttuvissa olosuhteissa
Szostoková, Kateřina. "Vztah mezi počtem druhů, teplotou, a úživností prostředí pro původní a nepůvodní druhy rostlin". Master's thesis, 2016. http://www.nusl.cz/ntk/nusl-345063.
Pełny tekst źródłaKsiążki na temat "Non-vascular plants"
Sorrie, Bruce A. The vascular and non-vascular flora of Nantucket, Tuckernuck, and Muskeget Islands. Nantucket, Mass: Massachusetts Audubon Society, 1996.
Znajdź pełny tekst źródłaProgram, Washington Natural Heritage, i Washington (State). Dept. of Natural Resources., red. Endangered, threatened & sensitive vascular plants of Washington: With working lists of rare non-vascular species. Wyd. 7. Olympia, Wash: Washington State Dept. of Natural Resources, 1997.
Znajdź pełny tekst źródłaA, Stapleton C., i Parks Canada Atlantic Region, red. The distribution and potential for invasiveness of some non-native vascular plants in Northern Cape Breton. Halifax, N.S: Parks Canada, Atlantic Region, 1998.
Znajdź pełny tekst źródłaGuidelines for Selection of Biological SSSIs: Non-vascular Plants. Joint Nature Conservation Committee, 1992.
Znajdź pełny tekst źródłaBronson, Vincent. Guide to Plant Athlete for Beginners: Plants Can Be Either Vascular or Non-Vascular. Independently Published, 2021.
Znajdź pełny tekst źródłaRayner, M. C. Mycorrhiza - An Account of Non-Pathogenic Infection by Fungi in Vascular Plants and Bryophytes. White Press, 2018.
Znajdź pełny tekst źródłaCzęści książek na temat "Non-vascular plants"
Kelcey, John G. "Plants (Non-vascular)". W Provisional Bibliography of Atlases, Floras and Faunas of European Cities: 1600–2014, 85–87. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-31120-3_7.
Pełny tekst źródłaOwfi, Reza E. "Cryptogamaes—Non-Vascular Plants". W Natural Products and Botanical Medicines of Iran, 219–26. First edition. | Boca Raton : CRC Press, 2020. | Series: Natural products chemistry of global plants: CRC Press, 2020. http://dx.doi.org/10.1201/9781003008996-8.
Pełny tekst źródłaPérez, Gisela Muro, Jaime Sánchez-Salas, Omag Cano-Villegas, Raúl López-García i Luis Manuel Valenzuela-Nuñez. "Introduction to Plant Taxonomy: Vascular and Non-vascular Plants with Medicinal Use". W Aromatic and Medicinal Plants of Drylands and Deserts, 1–6. Boca Raton: CRC Press, 2023. http://dx.doi.org/10.1201/9781003251255-1.
Pełny tekst źródłaRahmat, Somayeh. "Non-host Plant Species: Definition, Description, and Mechanisms of Interaction with Arbuscular Mycorrhizal Fungi". W Arbuscular Mycorrhizal Fungi and Higher Plants, 19–36. Singapore: Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-99-8220-2_2.
Pełny tekst źródłaLiénard, David, i Fabien Nogué. "Physcomitrella patens : A Non-Vascular Plant for Recombinant Protein Production". W Recombinant Proteins From Plants, 135–44. Totowa, NJ: Humana Press, 2009. http://dx.doi.org/10.1007/978-1-59745-407-0_8.
Pełny tekst źródłaMallick, N., i L. C. Rai. "Physiological Responses of Non-Vascular Plants to Heavy Metals". W Physiology and Biochemistry of Metal Toxicity and Tolerance in Plants, 111–47. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-017-2660-3_5.
Pełny tekst źródłaUpreti, D. K., i Rajesh Bajpai. "Status, Issues and Challenges of Biodiversity: Lower Plants (Non-vascular)". W Biodiversity in India: Status, Issues and Challenges, 15–24. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-9777-7_2.
Pełny tekst źródłaRapson, Gillian L. "At What Scales and in What Vegetation Types Should We Sample Non-vascular Plants?" W Vegetation Structure and Function at Multiple Spatial, Temporal and Conceptual Scales, 389–403. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-21452-8_17.
Pełny tekst źródłaFujinami, Rieko. "Analysis of Cell Division Frequency in the Root Apical Meristem of Lycophytes, Non-seed Vascular Plants, Using EdU Labeling". W Plant Stem Cells, 91–99. New York, NY: Springer US, 2019. http://dx.doi.org/10.1007/978-1-0716-0183-9_10.
Pełny tekst źródłaMüller, Norbert. "Most Frequently Occurring Vascular Plants and the Role of Non-Native Species in Urban Areas - A Comparison of Selected Cities in the Old and the New Worlds". W Urban Biodiversity and Design, 227–42. Oxford, UK: Wiley-Blackwell, 2010. http://dx.doi.org/10.1002/9781444318654.ch11.
Pełny tekst źródłaStreszczenia konferencji na temat "Non-vascular plants"
Stroock, Abraham D., Nak Won Choi, Tobias D. Wheeler, Valerie Cross, Scott Verbridge, Claudia Fischbach i Lawrence J. Bonassar. "Microvascular Structure and Function in Vitro". W ASME 2009 7th International Conference on Nanochannels, Microchannels, and Minichannels. ASMEDC, 2009. http://dx.doi.org/10.1115/icnmm2009-82124.
Pełny tekst źródłaBanaszek, Jarosław, Marzena Leksy i Oimahmad Rahmonov. "The Role of Spontaneous Succession in Reclamation of Mining Waste Tip in Area of Ruda Slaska City". W Environmental Engineering. VGTU Technika, 2017. http://dx.doi.org/10.3846/enviro.2017.098.
Pełny tekst źródłaEmerson, David R., i Robert W. Barber. "Designing Efficient Microvascular Networks Using Conventional Microfabrication Techniques". W ASME 2009 Second International Conference on Micro/Nanoscale Heat and Mass Transfer. ASMEDC, 2009. http://dx.doi.org/10.1115/mnhmt2009-18312.
Pełny tekst źródłaGhazali, Nurul Aimi, Shigemi Naganawa, Yoshihiro Masuda, Wan Asma Ibrahim i Noor Fitrah Abu Bakar. "Eco-Friendly Drilling Fluid Deflocculant for Drilling High Temperature Well: A Review". W ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-78149.
Pełny tekst źródłaRaporty organizacyjne na temat "Non-vascular plants"
Christopher, David A., i Avihai Danon. Plant Adaptation to Light Stress: Genetic Regulatory Mechanisms. United States Department of Agriculture, maj 2004. http://dx.doi.org/10.32747/2004.7586534.bard.
Pełny tekst źródłaBoyle, M. Terrestrial vegetation monitoring at Ocmulgee Mounds National Historical Park: 2021 data summary. National Park Service, lipiec 2023. http://dx.doi.org/10.36967/2299748.
Pełny tekst źródłaGranot, David, Richard Amasino i Avner Silber. Mutual effects of hexose phosphorylation enzymes and phosphorous on plant development. United States Department of Agriculture, styczeń 2006. http://dx.doi.org/10.32747/2006.7587223.bard.
Pełny tekst źródłaBoyle, M., i Elizabeth Rico. Terrestrial vegetation monitoring at Fort Matanzas National Monument: 2019 data summary. National Park Service, maj 2022. http://dx.doi.org/10.36967/nrds-2293409.
Pełny tekst źródłaBoyle, M., i Elizabeth Rico. Terrestrial vegetation monitoring at Cumberland Island National Seashore: 2020 data summary. National Park Service, wrzesień 2022. http://dx.doi.org/10.36967/2294287.
Pełny tekst źródłaBoyle, Maxwell. Terrestrial vegetation monitoring at Canaveral National Seashore: 2022 data summary. National Park Service, 2024. http://dx.doi.org/10.36967/2303291.
Pełny tekst źródłaBoyle, M. Terrestrial vegetation monitoring at Kennesaw Mountain National Battlefield Park: 2021 data summary. National Park Service, 2023. http://dx.doi.org/10.36967/2301001.
Pełny tekst źródłaBoyle, Maxwell, i Elizabeth Rico. Terrestrial vegetation monitoring at Fort Pulaski National Monument: 2019 data summary. National Park Service, grudzień 2021. http://dx.doi.org/10.36967/nrds-2288716.
Pełny tekst źródłaBoyle, M. Terrestrial vegetation monitoring at Chattahoochee River National Recreation Area: 2021 data summary. National Park Service, 2024. http://dx.doi.org/10.36967/2303257.
Pełny tekst źródłaBarg, Rivka, Erich Grotewold i Yechiam Salts. Regulation of Tomato Fruit Development by Interacting MYB Proteins. United States Department of Agriculture, styczeń 2012. http://dx.doi.org/10.32747/2012.7592647.bard.
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