dc.creatorMendoza, Ursula N.
dc.creatorCruz, Cleise Cordeiro da
dc.creatorMenezes, Moirah
dc.creatorLara, Ruben Jose
dc.date.accessioned2017-08-03T22:13:26Z
dc.date.accessioned2018-11-06T13:55:25Z
dc.date.available2017-08-03T22:13:26Z
dc.date.available2018-11-06T13:55:25Z
dc.date.created2017-08-03T22:13:26Z
dc.date.issued2011-10
dc.identifierMendoza, Ursula N.; Cruz, Cleise Cordeiro da ; Menezes, Moirah; Lara, Ruben Jose; Flooding effects on phosphorus dynamics in an Amazonian mangrove forest, Northern Brazil; Springer; Plant and Soil; 353; 1-2; 10-2011; 107-121
dc.identifier0032-079X
dc.identifierhttp://hdl.handle.net/11336/21856
dc.identifier1573-5036
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1880669
dc.description.abstractAims and methods We examined porewater salinity, soil redox potential (Eh), soil extractable phosphate (extr.-P), leaf phosphorus (leaf-P) and plant growth in relation to inundation frequency (IF) and mangrove species distributions along a 600 m transect in the Bragança Peninsula, North Brazil. Results The forest species composition changed across the tidal zone with Avicennia germinans dominating (99.1%) the high intertidal (HI) zone where the IF was 41–67 d.y−1 , Rhizophora mangle, Laguncularia racemosa and A. germinans co-occured in the mid intertidal (MI), and a mixed R. mangle (47.1%) - A, germinans (41.2%) stand occupied the low intertidal (LI) zone with an IF of 124–162 d.y−1 . Low IF resulted in high Eh levels (200 mV) in the HI zone relative to the LI where Eh ranged from 0–100 mV. The IF showed a significant positive correlation with extr.-P (r=0,89; p=0.05) and a negative association with Eh (r=−0,75; p=0.05). Conclusion An ANCOVA confirmed that Eh and extr.P were influenced by flooding. Variations in these factors were reflected in patterns of P leaf tissue concentrations across the gradient; however, a MANCOVA showed that leaf-P was not related to tree height, tree volume or basal area. Waterlogging conditions, porewater salinity, and P dynamics in the sediment appear to influence the forest structure. We suggest that P availability plays an important role in controling mangrove species distributions but not their growth.
dc.languageeng
dc.publisherSpringer
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s11104-011-1013-6
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs11104-011-1013-6
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectAmazonia
dc.subjectMangrove
dc.subjectInundation
dc.subjectPhosphorus
dc.subjectRedox potential
dc.titleFlooding effects on phosphorus dynamics in an Amazonian mangrove forest, Northern Brazil
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.typeArtículos de revistas


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