georefid:2010-044674SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-07-06T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1029/2007PA001473<gco:CharacterString>Magnetofossil spike during the Paleocene-Eocene Thermal Maximum; ferromagnetic resonance, rock magnetic, and electron microscopy evidence from Ancora, New Jersey, United States</gco:CharacterString>2007-01-01publicationgeorefid:2010-044674doi:10.1029/2007PA001473Kopp, Robert E.California Institute of Technology, Division of Geological and Planetary Sciences, Pasadena, CA, United StatesauthorRaub, Timothy D.Yale University, United StatesauthorSchumann, DirkMcGill University, CanadaauthorVali, HojatollahauthorSmirnov, Alexei V.authorKirschvink, Joseph L.authorAmerican Geophysical Union, Washington, DC, United StatespublisherdocumentDigitalPaleoceanography22 (4)completedStratigraphyAncora New Jerseyanhysteretic remanent magnetizationAtlantic Coastal Plainbacteriabiogenic processesCamden County New JerseyCenozoiccontinental margincoresEoceneexperimental studiesisothermal remanent magnetizationLeg 174AXlower Eocenemagnetic anomaliesmagnetitemagnetizationmagnetotactic taxaNew JerseyOcean Drilling Programoxidespaleo-oceanographyPaleocenePaleocene-Eocene Thermal MaximumpaleoclimatologypaleoecologyPaleogenepaleogeographypaleolatitudepaleomagnetismproductivityremanent magnetizationreversalssedimentsTEM dataTertiaryUnited Statesupper PaleoceneEnglishgeoscientificInformation-74.5056-74.505639.413239.4132Ancora New Jerseyapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www.agu.org/journals/pa/pa0704/2007PA001473/2007PA001473.pdfdownload