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{'doi': '10.2110/palo.2013.105', 'member_id': '860', 'member': 'Society for Sedimentary Geology', 'container-title': 'PALAIOS', 'primary-resource': 'https://pubs.geoscienceworld.org/palaios/article/29/6/266-276/146406', 'tld': 'geoscienceworld.org', 'clearbit-logo': 'https://logo.clearbit.com/geoscienceworld.org', 'coaccess': [], 'multiple-resolution': [{'url': 'http://palaios.geoscienceworld.org/cgi/doi/10.2110/palo.2013.105', 'tld': 'geoscienceworld.org', 'clearbit-logo': 'https://logo.clearbit.com/geoscienceworld.org'}], 'type': 'JOURNAL ARTICLE', 'published_date': '3 October 2014', 'publication': 'PALAIOS', 'supplementary_ids': None, 'title': 'MANGANESE-BEARING RHIZOCRETIONS IN THE WILLWOOD FORMATION, WYOMING, U.S.A.: IMPLICATIONS FOR PALEOCLIMATE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM', 'name': None, 'id': None, 'location': None, 'display_doi': 'https://doi.org/10.2110/palo.2013.105', 'grant_info': None, 'editors': None, 'authors': 'D. T. WOODY | J. J. SMITH | M. J. KRAUS | S. T. HASIOTIS', 'chairs': None}
https://doi.org/10.2110/palo.2013.105
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