Ornithopods

@misc{smith1984petroleum,
    author = "Smith, T. N.",
    title = "Petroleum development, North Slope of Alaska",
    year = "1984",
    url = "https://doi.org/10.14509/739",
    doi = "10.14509/739"
}

@incollection{crossref1985petroleum,
    title = "Petroleum Geochemistry of North Slope Alaska",
    year = "1985",
    booktitle = "Alaska North Slope Oil-Rock Correlation Study",
    url = "https://doi.org/10.1306/st20445c12",
    doi = "10.1306/st20445c12",
    pages = "243-279"
}

@article{mickey1985jurassicneocomian,
    author = "Mickey, M. B. and Haga, Hideyo",
    title = "Jurassic-Neocomian Biostratigraphy, North Slope, Alaska",
    year = "1985",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad4626a0-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad4626a0-16f7-11d7-8645000102c1865d",
    number = "4",
    pages = "669-669",
    volume = "69"
}

Abundant skeletal remains demonstrate that lambeosaurine hadrosaurid, tyrannosaurid, and troodontid dinosaurs lived on the Alaskan North Slope during late Campanian—early Maestrichtian time (about 66 to 76 million years ago) in a deltaic environment dominated by herbaceous vegetation. The high ground terrestrial plant community was a mild- to cold-temperate forest composed of coniferous and broad leaf trees. The high paleolatitude (about 70° to 85° North) implies extreme seasonal variation in solar insolation, temperature, and herbivore food supply. Great distances of migration to contemporaneous evergreen floras and the presence of both juvenile and adult hadrosaurs suggest that they remained at high latitudes year-round. This challenges the hypothesis that short-term periods of darkness and temperature decrease resulting from a bolide impact caused dinosaurian extinction.

@article{brouwers1987dinosaurs,
    author = "Brouwers, Elisabeth M. and Clemens, William A. and Spicer, Robert A. and Ager, Thomas A. and Carter, L. David and Sliter, William V.",
    title = "Dinosaurs on the North Slope, Alaska: High Latitude, Latest Cretaceous Environments",
    year = "1987",
    journal = "Science",
    abstract = "Abundant skeletal remains demonstrate that lambeosaurine hadrosaurid, tyrannosaurid, and troodontid dinosaurs lived on the Alaskan North Slope during late Campanian—early Maestrichtian time (about 66 to 76 million years ago) in a deltaic environment dominated by herbaceous vegetation. The high ground terrestrial plant community was a mild- to cold-temperate forest composed of coniferous and broad leaf trees. The high paleolatitude (about 70° to 85° North) implies extreme seasonal variation in solar insolation, temperature, and herbivore food supply. Great distances of migration to contemporaneous evergreen floras and the presence of both juvenile and adult hadrosaurs suggest that they remained at high latitudes year-round. This challenges the hypothesis that short-term periods of darkness and temperature decrease resulting from a bolide impact caused dinosaurian extinction.",
    url = "https://doi.org/10.1126/science.237.4822.1608",
    doi = "10.1126/science.237.4822.1608",
    number = "4822",
    pages = "1608-1610",
    volume = "237"
}

Hadrosaur Bones have been found on the Colville River north of Umiat on the North Slope of Alaska. This find represents the first report of dinosaur bones in Alaska and their northernmost reported occurrence. The remains are not determinable below family level but are important, nonetheless, for interpretations of the paleoclimatology and paleobiogeography of the Late Cretaceous.

@article{davies1987duckbill,
    author = "Davies, Kyle L.",
    title = "Duck-bill dinosaurs (Hadrosauridae, Ornithischia) from the North Slope of Alaska",
    year = "1987",
    journal = "Journal of Paleontology",
    abstract = "Hadrosaur Bones have been found on the Colville River north of Umiat on the North Slope of Alaska. This find represents the first report of dinosaur bones in Alaska and their northernmost reported occurrence. The remains are not determinable below family level but are important, nonetheless, for interpretations of the paleoclimatology and paleobiogeography of the Late Cretaceous.",
    url = "https://doi.org/10.1017/s0022336000028341",
    doi = "10.1017/s0022336000028341",
    number = "1",
    pages = "198-200",
    volume = "61"
}

@article{davies1987duckbill1,
    author = "Davies, K. L",
    title = "Duckbill dinosaurs from the North Slope of Alaska",
    year = "1987",
    journal = "Journal of Paleontology, v. 61, p. 198-200",
    note = "talkorigins\_source = {true}; raw\_reference = {Davies, K. L., 1987, Duckbill dinosaurs from the North Slope of Alaska: Journal of Paleontology, v. 61, p. 198-200.}"
}

@misc{binnian2005beaufort,
    author = "Binnian, Emily F.",
    title = "Beaufort Coastal Plain, North Slope, Alaska",
    year = "2005",
    booktitle = "Fact Sheet",
    url = "https://doi.org/10.3133/fs20053007",
    doi = "10.3133/fs20053007"
}

@misc{helsel2016north,
    author = "Helsel, Frederick and Dexheimer, Darielle and Lucero, Daniel",
    title = "North Slope of Alaska ARM Facilities.",
    year = "2016",
    url = "https://doi.org/10.2172/1431186",
    doi = "10.2172/1431186"
}

@book{fiorillo2018alaska,
    author = "Fiorillo, Anthony R.",
    title = "Alaska Dinosaurs",
    year = "2018",
    url = "https://doi.org/10.1201/b22215",
    doi = "10.1201/b22215"
}

@incollection{bart20194,
    author = "Bart, Jonathan and Brown, Stephen and Andres, Brad A. and Platte, Robert and Manning, Ann",
    title = "4. NORTH SLOPE OF ALASKA",
    year = "2019",
    booktitle = "Arctic Shorebirds in North America",
    url = "https://doi.org/10.1525/9780520953499-006",
    doi = "10.1525/9780520953499-006",
    pages = "37-96"
}

@incollection{birdNonenorth,
    author = "Bird, Kenneth J.",
    title = "North Slope of Alaska",
    year = "None",
    booktitle = "Economic Geology, U.S.",
    url = "https://doi.org/10.1130/dnag-gna-p2.447",
    doi = "10.1130/dnag-gna-p2.447",
    pages = "447-462"
}