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008 150903s2006 ne | o |||| 0|eng d
020 _a9781402044434
_99781402044434
024 7 _a10.1007/9781402044434
_2doi
035 _avtls000334769
039 9 _a201509030248
_bVLOAD
_c201404300255
_dVLOAD
_y201402041157
_zstaff
040 _aMX-SnUAN
_bspa
_cMX-SnUAN
_erda
050 4 _aQH540-549.5
100 1 _aRozema, Jelte.
_eeditor.
_9309635
245 1 0 _aPlants and Climate Change /
_cedited by Jelte Rozema, Rien Aerts, Hans Cornelissen.
264 1 _aDordrecht :
_bSpringer Netherlands,
_c2006.
300 _aviii, 264 páginas
_brecurso en línea.
336 _atexto
_btxt
_2rdacontent
337 _acomputadora
_bc
_2rdamedia
338 _arecurso en línea
_bcr
_2rdacarrier
347 _aarchivo de texto
_bPDF
_2rda
490 0 _aTasks for vegetation science ;
_v41
500 _aSpringer eBooks
505 0 _aGlobal climate change: atmospheric CO2 enrichment, global warming and stratospheric ozone depletion -- Responses of terrestrial Antarctic ecosystems to climate change -- Atmospheric CO2 enrichment -- Vascular plant responses to elevated CO2 in a temperate lowland Sphagnum peatland -- Moss responses to elevated CO2 and variation in hydrology in a temperate lowland peatland -- From transient to steady-state response of ecosystems to atmospheric CO2-enrichment and global climate change: conceptual challenges and need for an integrated approach -- Plant performance in a warmer world: general responses of plants from cold, northern biomes and the importance of winter and spring events -- Global warming -- Stable isotope ratios as a tool for assessing changes in carbon and nutrient sources in Antarctic terrestrial ecosystems -- Upscaling regional emissions of greenhouse gases from rice cultivation: methods and sources of uncertainty -- Stratospheric ozone depletion -- Effects of enhanced UV-B radiation on nitrogen fixation in arctic ecosystems -- Stratospheric ozone depletion: high arctic tundra plant growth on Svalbard is not affected by enhanced UV-B after 7 years of UV-B supplementation in the field -- Outdoor studies on the effects of solar UV-B on bryophytes: overview and methodology -- Reconstruction of Past Climates using plant derived proxies -- A vegetation, climate and environment reconstruction based on palynological analyses of high arctic tundra peat cores (5000–6000 years BP) from Svalbard -- Physiognomic and chemical characters in wood as palaeoclimate proxies -- The occurrence of p-coumaric acid and ferulic acid in fossil plant materials and their use as UV-proxy -- Biomacromolecules of algae and plants and their fossil analogues.
520 _aThe book Plants and Climate Change focuses on how climate affects or affected the biosphere and vice versa both in the present and past. The chapters describe how ecosystems from the Antarctic and arctic and from other latitudes respond to global climate change. The book covers papers highlighting plant responses to atmospheric CO2 increase, to global warming and to increased ultraviolet-B radiation as a result of stratospheric ozone depletion. Depending on how and how well plant responses to increased temperature, atmospheric CO2 and ultraviolet-B have been preserved in the (sub)-fossil record, past climates and past atmospheric chemistry may be reconstructed. Pollen and tree-ring data reflect plant species composition and variation of temperature and precipitation over long or shorter time intervals. In addition to well preserved morphological and chemical plant properties, new analytical techniques such as stable isotopes are becoming increasingly important in this respect. The development and validation of such biotic climate and environment proxies build a bridge between biological and geological research. This highlights that plant-climate change research is becoming a multi- and transdisciplinary field of relevant research. Reprinted from Plant Ecology, 182:1-2 (2006).
590 _aPara consulta fuera de la UANL se requiere clave de acceso remoto.
700 1 _aAerts, Rien.
_eeditor.
_9309636
700 1 _aCornelissen, Hans.
_eeditor.
_9309637
710 2 _aSpringerLink (Servicio en línea)
_9299170
776 0 8 _iEdición impresa:
_z9781402044427
856 4 0 _uhttp://remoto.dgb.uanl.mx/login?url=http://dx.doi.org/10.1007/978-1-4020-4443-4
_zConectar a Springer E-Books (Para consulta externa se requiere previa autentificación en Biblioteca Digital UANL)
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999 _c282694
_d282694