Lateral inputs drive subsurface carbon export in the equatorial Atlantic during the low-productivity period.

Joelle Habib1,2, Lars Stemmann1, Peter Brandt2, Ana Fernández-Carrera3, Franz Philip Tuchen4, Ajit Subramaniam5, Alberto Baudena6, Wokil Bam7, Claudeilton de Santana8, Beat Gasser9 and Rainer Kiko1,2, (1)Laboratoire d'Océanographie de Villefranche, Villefranche-sur-Mer, France, (2)GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany, (3)Universidad de Las Palmas de Gran Canaria, Gran Canaria, Spain, (4)Institute of Environmental Physics, University of Bremen, Bremen, Germany, (5)Columbia University, New York, United States, (6)Consiglio Nazionale Delle Ricerche- Istituto di Scienze Marine (CNR-ISMAR), Lerici, Italy, (7)Woods Hole Oceanographic Institution, Department of Marine Chemistry & Geochemistry, Woods Hole, United States, (8)GEOMAR Helmholtz Centre for Ocean Research Kiel, RD2 - Plankton Biogeochemistry and Dynamics, Kiel, Germany, (9)IAEA, Monaco, Monaco