2016
DOI: 10.1016/j.ecss.2015.12.024
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Origin, composition and quality of suspended particulate organic matter in relation to freshwater inflow in a South Texas estuary

Abstract: HAL is a multidisciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L'archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d'enseignement et de recherche français ou étrangers, des labora… Show more

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Cited by 45 publications
(29 citation statements)
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“…Riverine δ 13 C-DIC can drive down the estuarine δ 13 C-POC through uptake and fixation by estuarine phytoplankton (Figure 4B; Fogel et al, 1992). Delivery of freshwater phytoplankton from the rivers to the bay may also have contributed to the lower δ 13 C signal that we observed (δ 13 C = −31.4 , Lebreton et al, 2016). While depleted δ 13 C values in river water are often attributed to C3 plant contributions from the surrounding terrestrial landscape, this is not a viable explanation in this system because POM in the Mission and Aransas rivers becomes enriched in δ 13 C-POC during storm flow conditions (δ 13 C = −22 to −20 , Mooney and McClelland, 2012).…”
Section: Discussion Pom Source Following Storm Eventscontrasting
confidence: 43%
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“…Riverine δ 13 C-DIC can drive down the estuarine δ 13 C-POC through uptake and fixation by estuarine phytoplankton (Figure 4B; Fogel et al, 1992). Delivery of freshwater phytoplankton from the rivers to the bay may also have contributed to the lower δ 13 C signal that we observed (δ 13 C = −31.4 , Lebreton et al, 2016). While depleted δ 13 C values in river water are often attributed to C3 plant contributions from the surrounding terrestrial landscape, this is not a viable explanation in this system because POM in the Mission and Aransas rivers becomes enriched in δ 13 C-POC during storm flow conditions (δ 13 C = −22 to −20 , Mooney and McClelland, 2012).…”
Section: Discussion Pom Source Following Storm Eventscontrasting
confidence: 43%
“…Freshwater discharge into the MAE has been variable over the past decade; multi-year droughts with very low baseflows are interspersed with large storm events occurring at high frequency for many months at a time, as seen during the study period (Figure 2A) and in previous studies (Mooney and McClelland, 2012;Bruesewitz et al, 2013;Lebreton et al, 2016). These sporadic freshwater inflows significantly influence system-wide salinity, with a decreasing degree of influence along the inshore to offshore transect ( Figure 2B).…”
Section: Discussion Pom Source Following Storm Eventsmentioning
confidence: 77%
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“…For instance, Venkataramana et al [12] projected multi-year droughts in the late 21st century to occur across the state, with the worst droughts anticipated in El Paso. Effects of severe drought conditions on dissolved organic matter and ecosystems have been estimated by Miller and Shank [13], Acosta-Martinez et al [14], Lebreton et al [15], and Schwantes et al [16]. Specifically, the 2011 drought has accounted for considerable losses in agricultural production of $7.62 billion in Texas (not including timber production) [1,2,17].…”
Section: Introductionmentioning
confidence: 99%