http://www.cnr.it/ontology/cnr/individuo/prodotto/ID42436
Dissolved organic matter composition in a fragmented Mediterranean fluvial system under severe drought conditions (Articolo in rivista)
- Type
- Label
- Dissolved organic matter composition in a fragmented Mediterranean fluvial system under severe drought conditions (Articolo in rivista) (literal)
- Anno
- 2011-01-01T00:00:00+01:00 (literal)
- Alternative label
Vasquez E., Amalfitano S., Fazi A., Butturini A. (2011)
Dissolved organic matter composition in a fragmented Mediterranean fluvial system under severe drought conditions
in Biogeochemistry (Dordrecht)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Vasquez E., Amalfitano S., Fazi A., Butturini A. (literal)
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- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Departament d'Ecologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain
Istituto di Ricerca sulle Acque (IRSA-CNR), Area della Ricerca ''Roma 1'', Via Salaria km 29,300, CP1000016 Monterotondo, Rome, Italy (literal)
- Titolo
- Dissolved organic matter composition in a fragmented Mediterranean fluvial system under severe drought conditions (literal)
- Abstract
- Abstract In Mediterranean regions, drought is one of
the main factors shaping fluvial ecosystems. Droughts
cause a shift from lotic to lentic conditions, triggering a
gradual fragmentation of the longitudinal hydrological
continuum, and a severe alteration of water chemical
properties. However, within a biogeochemical perspective,
little is known about how and to which extend
droughts modify the chemical properties of dissolved
organic matter (DOM). In this study, the variability of
DOM properties along a fragmented fluvial system is
explored, during a summer severe drought, by means of
(a) the ratio between dissolved organic carbon and
nitrogen concentrations (DOC:DON); (b) DOC bioavailability
(BDOC) and (c) DOM optical properties
(SUVA index, fluorescence index, and excitation-
emission fluorescence matrices). DOM and water
measurements were collected from isolated water
parcels that became disconnected from the fluvial
continuum at different times, and were compared with
data obtained in the following autumn, when the fluvial
continuum was re-established. Analysis of DOM
chemical properties evidenced that these properties
during drought clearly differed from those observed in
autumn, but changes did not follow an arbitrary pattern.
Thus, the sampling sites with lotic water bodies showed
DOM properties similar to those observed in autumn
reflecting the dominance of terrestrial inputs. But, once
hydrological fragmentation occurred, there was a gradual
increase in the contribution of autochthonous DOM
as the time elapsed since the poolswere established, and
the geochemical conditions shifted from oxidized
to reduced conditions. In consequence, the fragmentation
of fluvial continuum generates a set of distinct
biochemical hot spots (i.e., each water parcel),
revealing that extreme drought greatly amplifies the
qualitative heterogeneity of organicmatter in a fluvial
system. (literal)
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