Use of multiple oxygen isotope proxies for elucidating Arctic Cretaceous palaeo-hydrology

• Main Authors: Celina A. Suarez, G. A. Ludvigson, L. A. Gonzalez, A. R. Fiorillo, P. P. Flaig, P. J. McCarthy
• Format: Dataset
• Language: unknown
• Published: 2016
• Subjects: Geology; 6.3; Ancestral Brooks Range; oxygen isotope proxies; Cretaceous; body temperatures; Brooks Range; Ingested water compositions; proxy; circulation models; siderite; δ 18 O; dinosaur tooth enamel phosphate; dinosaur teeth; corroborating evidence; rainout effects; hydrological cycle; USA; Colville Basin; Arctic; Prince Creek; Alaska
• Online Access: https://doi.org/10.6084/m9.figshare.3453407.v1; https://figshare.com/articles/Use_of_multiple_oxygen_isotope_proxies_for_elucidating_Arctic_Cretaceous_palaeo-hydrology/3453407

Stable oxygen isotope analysis of siderite and dinosaur tooth enamel phosphate from the Campanian–Maastrichtian Prince Creek Formation, Alaska, USA, are analysed to determine the palaeohydrology of the ancient Colville Basin north of the Ancestral Brooks Range. δ 18 O of freshwater siderites relative to V-PDB ranges between −14.86 and −16.21‰. Dinosaur tooth enamel δ 18 O from three different sites (Kikak–Tegoseak, Pediomys Point, Liscomb) range between +3.9‰ and +10.2.0‰. δ 18 O meteoric water are calculated from δ 18 O siderite that formed at seasonal temperatures ranging from −2 to 14.5 °C, with a mean annual temperature of 6.3 °C. At 6.3 °C, the δ 18 O w calculated from siderite ranged between −22.23 and −20.89‰ V-SMOW. Ingested water compositions are estimated from dinosaur teeth assuming body temperatures of 37 °C and local relative humidity of 77.5%, resulting in values ranging from −28.7 to −20.4‰ V-SMOW, suggesting consumption of meteoric water and orographically depleted runoff from the Brooks Range. The ranges in calculated δ 18 O meteoric water are compatible between the two proxies, and are mutually corroborating evidence of extremely 18 O-depleted precipitation at high latitudes during the Late Cretaceous relative to those generated using general circulation models. This depletion is proposed to result from increased rainout effects from an intensified hydrological cycle, which probably played a role in sustaining polar warmth.