Miocene to Holocene marine tephrostratigraphy offshore northern Central America and southern Mexico: Pulsed activity of known volcanic complexes Schindlbeck, J.C.1, Kutterolf, S.2, Freundt, A.2, Eisele, S. 3, Wang, K.-L.4,5, Frische, M.2 1Heidelberg University, Institute of Earth Sciences, Im Neuenheimer Feld 234-236, 69120 Heidelberg, Germany 2GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany 3 Asian School of the Environment, Nanyang Technological University, Singapore 4Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan 5Department of Geosciences, National Taiwan University, Taipei 106, Taiwan Corresponding author: Julie C. Schindlbeck (
[email protected]) Key Points: Stratigraphically classified tephra database of glass compositions with correlations of marine and terrestrial tephra layers New insights into the lifetime of the major volcanic centers in Guatemala and El Salvador and their number of major eruptions Identification of five pulses of enhanced volcanic activity during the Quaternary, the Pliocene, the Late, Middle Miocene and Early This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1029/2018GC007832 © 2018 American Geophysical Union. All rights reserved. Abstract We studied the tephra inventory of fourteen deep sea drill sites of three DSDP and ODP legs drilled offshore Guatemala and El Salvador (Legs 67, 84, 138), and one leg offshore Mexico (Leg 66). Marine tephra layers reach back from the Miocene to the Holocene. We identified 223 primary ash beds and correlated these between the drill sites, with regions along the volcanic arcs, and to specific eruptions known from land.