<?xml version="1.0" encoding="UTF-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcq="http://purl.org/dc/terms/"><records count="1" morepages="false" start="1" end="1"><record rownumber="1"><dc:product_type>Journal Article</dc:product_type><dc:title>Mechanisms Driving the Dispersal of Hydrothermal Iron From the Northern Mid Atlantic Ridge</dc:title><dc:creator>Tagliabue, Alessandro; Lough, Alastair J.; Vic, Clément; Roussenov, Vassil; Gula, Jonathan; Lohan, Maeve C.; Resing, Joseph A.; Williams, Richard G.</dc:creator><dc:corporate_author/><dc:editor/><dc:description>Key Points                                                            Iron is dispersed from trans Atlantic geotraverse predominantly northward within the axial valley and westward off axis, dominated by the colloidal size fraction                                                  A combination of fine‐scale processes are necessary to explain the dispersal both within and outside the axial valley                                                  Coarse resolution models are impaired in their ability to constrain the broader influence of iron supplied from axial valley ridge systems</dc:description><dc:publisher/><dc:date>2022-11-28</dc:date><dc:nsf_par_id>10443586</dc:nsf_par_id><dc:journal_name>Geophysical Research Letters</dc:journal_name><dc:journal_volume>49</dc:journal_volume><dc:journal_issue>22</dc:journal_issue><dc:page_range_or_elocation/><dc:issn>0094-8276</dc:issn><dc:isbn/><dc:doi>https://doi.org/10.1029/2022GL100615</dc:doi><dcq:identifierAwardId>1840868</dcq:identifierAwardId><dc:subject/><dc:version_number/><dc:location/><dc:rights/><dc:institution/><dc:sponsoring_org>National Science Foundation</dc:sponsoring_org></record></records></rdf:RDF>