Articles | Volume 6, issue 2
https://doi.org/10.5194/gchron-6-125-2024
https://doi.org/10.5194/gchron-6-125-2024
Research article
 | 
17 Apr 2024
Research article |  | 17 Apr 2024

Evaluating manual versus automated benthic foraminiferal δ18O alignment techniques for developing chronostratigraphies in marine sediment records

Jennifer L. Middleton, Julia Gottschalk, Gisela Winckler, Jean Hanley, Carol Knudson, Jesse R. Farmer, Frank Lamy, Lorraine E. Lisiecki, and Expedition 383 Scientists

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Cited articles

Ahn, S., Khider, D., Lisiecki, L. E., and Lawrence, C. E.: A probabilistic Pliocene–Pleistocene stack of benthic δ18O using a profile hidden Markov model, Dynamics and Statistics of the Climate System, 2, dzx002, https://doi.org/10.1093/climsys/dzx002, 2017. 
Berger, A. and Loutre, M. F.: New Insolation values for the climate of the last 10 million years, Scientific Report 1988/13, Institute d'Astronomie et de Geophysique Georges Lemaitre, Universite Catholique de Louvain-la-Neuve, 1988. 
Bickert, T., Curry, W., and Wefer, G.: Late Pliocene to Holocene (2.6–0 Ma) western equatorial Atlantic deep-water circulation: Inferences from benthic stable isotopes, Proceedings of the Ocean Drilling Program, Scientific Results, 154, 239–254, 1997. 
Billups, K., Ravelo, A. C., and Zachos, J. C.: Early Pliocene deep water circulation in the western equatorial Atlantic: Implications for high-latitude cliamte change, Paleoceanography, 13, 84–95, 1998. 
Channell, J. E. T. and Raymo, M. E.: Paleomagnetic record at ODP Site 980 (Feni Drift, Rockall) for the past 1.2 Myrs, Geochem. Geophy., 4, 1033, https://doi.org/10.1029/2002GC000440, 2003. 
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We present oxygen isotope data for a new sediment core from the South Pacific and assign ages to our record by aligning distinct patterns in observed oxygen isotope changes to independently dated target records with the same patterns. We examine the age uncertainties associated with this approach caused by human vs. automated alignment and the sensitivity of outcomes to the choice of alignment target. These efforts help us understand the timing of past climate changes.
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