[
    {
        "id": "authors:tcnyp-x4g68",
        "collection": "authors",
        "collection_id": "tcnyp-x4g68",
        "cite_using_url": "https://resolver.caltech.edu/CaltechAUTHORS:20200220-072920683",
        "type": "article",
        "title": "The Occurrence of Flints and Extinct Animals in Pluvial Deposits near Clovis, New Mexico. Part III: Geology and Vertebrate Paleontology of the Late Quaternary near Clovis, New Mexico",
        "author": [
            {
                "family_name": "Stock",
                "given_name": "Chester",
                "clpid": "Stock-C"
            },
            {
                "family_name": "Bode",
                "given_name": "Francis D.",
                "clpid": "Bode-F-D"
            }
        ],
        "abstract": "At the suggestion of Dr. John C. Merriam and with the support of the Carnegie Institution of Washington, a field party from the California Institute of Technology co6perated with Dr. Edgar B. Howard in the investigation of late Quaternary sediments containing artifacts and remains of extinct mammals near Clovis, New Mexico. Field work was conducted in this region during the summer of 1933. The primary purposes of the present study were to locate accurately the occurrences of remains of mammals with reference to the position of artifacts and other evidences of the presence of early Man in the deposits, to identify the kinds of mammals represented, to determine the nature of the deposits themselves, and to establish, if possible, the conditions under which sediments and organic record accumulated. During the progress of this work in the field, critical localities were examined, and the problem of early Man in this region was discussed by members of the XVI International Geological Congress including Sir Arthur Smith Woodward and Lady Woodward, Dr. Victor Van Straelen, and Dr. John C. Merriam. It is a pleasure to acknowledge the expressions of opinion rendered by members of this group during and after examination of the field evidence.",
        "issn": "0097-3157",
        "publisher": "Academy of Natural Sciences",
        "publication": "Proceedings of the Academy of Natural Sciences of Philadelphia",
        "publication_date": "1936-06-15",
        "volume": "88",
        "pages": "219-241"
    },
    {
        "id": "authors:q962t-w4524",
        "collection": "authors",
        "collection_id": "q962t-w4524",
        "cite_using_url": "https://resolver.caltech.edu/CaltechAUTHORS:STOpnas35d",
        "type": "article",
        "title": "Occurrence of lower Oligocene mammal-bearing beds near Death Valley, California",
        "author": [
            {
                "family_name": "Stock",
                "given_name": "Chester",
                "clpid": "Stock-C"
            },
            {
                "family_name": "Bode",
                "given_name": "Francis D.",
                "clpid": "Bode-F-D"
            }
        ],
        "abstract": "It is a curious fact that while the White River deposits with their wealth of vertebrate fossils are widely distributed in the western Great Plains and occur also in certain of the intermontane basins of the Cordilleran province, no horizon, recognized on the basis of land mammals as equivalent in time to the lower Oligocene or Titanotherium Zone, has been found beyond these areas on the North American continent.(1) All the more unusual does this fact seem when it is realized that since the definition of the White River Group by Hayden in 1862 and the early researches on the White River fossil vertebrates by Leidy, Cope and Marsh, field investigations in the Tertiary have progressed broadly and intensively over the Far West.",
        "doi": "10.1073/pnas.21.10.571",
        "issn": "0027-8424",
        "publisher": "National Academy of Sciences",
        "publication": "Proceedings of the National Academy of Sciences of the United States of America",
        "publication_date": "1935-10",
        "series_number": "10",
        "volume": "21",
        "issue": "10",
        "pages": "571-579"
    },
    {
        "id": "authors:hxftc-x9935",
        "collection": "authors",
        "collection_id": "hxftc-x9935",
        "cite_using_url": "https://resolver.caltech.edu/CaltechAUTHORS:20191108-093248978",
        "type": "article",
        "title": "Characters Useful in Determining the Position of Individual Teeth in the Permanent Cheek-Tooth Series of Merychippine Horses",
        "author": [
            {
                "family_name": "Bode",
                "given_name": "Francis D.",
                "clpid": "Bode-F-D"
            }
        ],
        "abstract": "Cheek-teeth of fossil horses display structural characters long been recognized as of considerable value in establishing relationships of these forms and in furnishing suggestions as of the deposits in which the fossils occur. In later Cenozoic of western North America where complete skulls and skeletal are not always available, identification of members of the often based on single teeth.",
        "doi": "10.2307/1373910",
        "issn": "0022-2372",
        "publisher": "Oxford University Press",
        "publication": "Journal of Mammalogy",
        "publication_date": "1931-05-14",
        "series_number": "2",
        "volume": "12",
        "issue": "2",
        "pages": "118-129"
    }
]