<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Seasonal dissolved rare earth element dynamics of the Amazon River main stem, its tributaries, and the Curuai floodplain - art. no. Q12005</dc:title>
  <dc:creator>/Barroux, Gw&#xE9;na&#xEB;l</dc:creator>
  <dc:creator>Sonke, J. E.</dc:creator>
  <dc:creator>Boaventura, G.</dc:creator>
  <dc:creator>Viers, J.</dc:creator>
  <dc:creator>Godderis, Y.</dc:creator>
  <dc:creator>/Bonnet, Marie-Paule</dc:creator>
  <dc:creator>/Sondag, Francis</dc:creator>
  <dc:creator>Gardoll, S.</dc:creator>
  <dc:creator>/Lagane, Christelle</dc:creator>
  <dc:creator>/Seyler, Patrick</dc:creator>
  <dc:subject>rare earth element</dc:subject>
  <dc:subject>Amazon River</dc:subject>
  <dc:subject>neodymium</dc:subject>
  <dc:subject>mass balance</dc:subject>
  <dc:subject>floodplains</dc:subject>
  <dc:subject>tributaries</dc:subject>
  <dc:subject>geochemical cycles</dc:subject>
  <dc:subject>composition of the hydrosphere</dc:subject>
  <dc:subject>major and trace element geochemistry</dc:subject>
  <dc:description>We present a comprehensive dissolved rare earth element (REE) data set for the Amazon River and its main tributaries, Rio Negro, Solimoes, and Madeira, as well as the Curuai floodplain. The two-year time series show that REE vary seasonally with discharge in each of the tributaries, and indicate a hydrologically dominated control. Upper crust normalized REE patterns are relatively constant throughout the year, with Ce/Ce* anomalies being positively related to discharge. We propose revised annual dissolved REE fluxes to the surface Atlantic Ocean based on an integration of the seasonal data. For Nd (&lt; 0.22 mu m) this results in an average flux of 607 +/- 43 T/yr, which is at least 1.6 times larger than the previous estimate of 374 T/yr (&lt; 0.45 mu m) based on low water stage data. Moreover, during the high water season the maximum Nd flux measures 1277 t. yr(-1), constituting 30% of the required flux to the Atlantic Ocean (Tachikawa et al., 2003). Consequently, a smaller contribution of Nd from atmospheric and river particle desorption is required than was previously suggested. A mass balance of Amazon tributaries and observed fluxes at Obidos indicates that dissolved LREE behave quasi-conservatively. Conversely, the HREE mass balance presents a deficit during the high water stages, which could be related to the passage of water through the floodplain system accompanied by solid/dissolved phase transfer.</dc:description>
  <dc:date>2006</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010084910</dc:identifier>
  <dc:identifier>fdi:010084910</dc:identifier>
  <dc:identifier>Barroux Gw&#xE9;na&#xEB;l, Sonke J. E., Boaventura G., Viers J., Godderis Y., Bonnet Marie-Paule, Sondag Francis, Gardoll S., Lagane Christelle, Seyler Patrick. Seasonal dissolved rare earth element dynamics of the Amazon River main stem, its tributaries, and the Curuai floodplain - art. no. Q12005. 2006, 7,  NIL_37-NIL_54</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>BRESIL</dc:coverage>
  <dc:coverage>AMAZONIE</dc:coverage>
</oai_dc:dc>
