001     43975
005     20180210141801.0
024 7 _ |2 pmid
|a pmid:16435279
024 7 _ |2 DOI
|a 10.1055/s-2005-873008
024 7 _ |2 WOS
|a WOS:000235078600016
037 _ _ |a PreJuSER-43975
041 _ _ |a eng
082 _ _ |a 580
084 _ _ |2 WoS
|a Plant Sciences
100 1 _ |a Rascher, U.
|b 0
|u FZJ
|0 P:(DE-Juel1)129388
245 _ _ |a The "Kluge-Lüttge Kammer": a preliminary evaluation of an enclosed, crassulacean acid metabolism (CAM) mesocosm that allows separation of synchronized and desynchronized contributions of plants to whole system gas exchange
260 _ _ |a Oxford [u.a.] :Wiley- Blackwell
|b Wiley-Blackwell - STM
|c 2006
300 _ _ |a 167 - 174
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Plant Biology
|x 1435-8603
|0 10981
|y 1
|v 8
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Crassulacean acid metabolism (CAM) is recognized as a photosynthetic adaptation of plants to arid habitats. This paper presents a proof-of-concept evaluation of partitioning net CO2 exchanges for soil and plants in an arid, exclusively CAM mesocosm, with soil depth and succulent plant biomass approximating that of natural Sonoran Desert ecosystems. We present the first evidence that an enclosed CAM-dominated soil and plant community exposed to a substantial day/night temperature difference (30/20 degrees C), exhibits a diel gas exchange pattern consisting of four consecutive phases with a distinct nocturnal CO2 uptake. These phases were modulated by plant assimilation and soil respiration processes. Day-time stomatal closure of the CAM cycle during phase III was used to eliminate aboveground photosynthetic assimilation and respiration and thereby to estimate belowground plant plus soil respiration. Rapid changes in temperature appeared to synchronize single plant gas exchange but individual plant gas exchange patterns were desynchronized at constant day/night temperatures (25 degrees C), masking the distinct mesocosm pattern. Overall, the mean carbon budget of this CAM model Sonoran Desert system was negative, releasing an average of 22.5 mmol CO2 m-2 d-1. The capacity for nocturnal CO2 assimilation in this exclusively CAM mesocosm was inadequate to recycle CO2 released by plant and soil respiration.
536 _ _ |a Terrestrische Umwelt
|c P24
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK407
|x 0
588 _ _ |a Dataset connected to Web of Science, Pubmed
650 _ 2 |2 MeSH
|a Agave: metabolism
650 _ 2 |2 MeSH
|a Cactaceae: metabolism
650 _ 2 |2 MeSH
|a Carbon Dioxide: metabolism
650 _ 2 |2 MeSH
|a Circadian Rhythm
650 _ 2 |2 MeSH
|a Desert Climate
650 _ 2 |2 MeSH
|a Ecological Systems, Closed
650 _ 2 |2 MeSH
|a Photosynthesis
650 _ 2 |2 MeSH
|a Soil
650 _ 7 |0 0
|2 NLM Chemicals
|a Soil
650 _ 7 |0 124-38-9
|2 NLM Chemicals
|a Carbon Dioxide
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a Agave schottii
653 2 0 |2 Author
|a Opuntia engelmannii
653 2 0 |2 Author
|a gas exchange
653 2 0 |2 Author
|a Ferocactus wislizeni
653 2 0 |2 Author
|a mesocosm
653 2 0 |2 Author
|a Cylindropuntia versicolor
653 2 0 |2 Author
|a Crassulacean acid metabolism (CAM)
653 2 0 |2 Author
|a Camegiea gigantea
700 1 _ |a Bobich, E. G.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Osmond, C. B.
|b 2
|0 P:(DE-HGF)0
773 _ _ |a 10.1055/s-2005-873008
|g Vol. 8, p. 167 - 174
|p 167 - 174
|q 8<167 - 174
|0 PERI:(DE-600)2026390-9
|t Plant biology
|v 8
|y 2006
|x 1435-8603
909 C O |o oai:juser.fz-juelich.de:43975
|p VDB
913 1 _ |k P24
|v Terrestrische Umwelt
|l Terrestrische Umwelt
|b Erde und Umwelt
|0 G:(DE-Juel1)FUEK407
|x 0
914 1 _ |y 2006
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-III
|l Phytosphäre
|d 31.12.2006
|g ICG
|0 I:(DE-Juel1)VDB49
|x 0
970 _ _ |a VDB:(DE-Juel1)62066
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IBG-2-20101118
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-2-20101118
981 _ _ |a I:(DE-Juel1)ICG-3-20090406


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