220 Year Diatom δ18O Reconstruction of the Guaymas Basin Thermocline Using Microfluorination. Issue 2 (31st January 2020)

• Record Type: Journal Article
• Authors: Menicucci, Anthony J.; Thunell, Robert C.; Spero, Howard J.
• Is Part Of: Paleoceanography and paleoclimatology. Volume 35:Issue 2(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-01-31
• Subjects: Diatoms -- Guaymas basin -- sediment trap -- microfluorination -- oxygen isotopes; Paleoceanography -- Periodicals; Paleoclimatology -- Periodicals; 551.46
• DOI: 10.1029/2019PA003749
• Languages: English
• ISSNs: 2572-4517

Abstract

Abstract: The removal of exchangeable oxygen from diatom opal prior to δ 18 Odiatom analysis is a crucial first step before analyzing frustule oxygen isotopes for paleoceanographic applications. We present the results of experiments that quantify the temperature‐dependent reactivity of biogenic silica with water under laboratory conditions. We demonstrate that controlled exchange between rinse water and diatom opal at room temperature results in predictable alteration of δ 18 Odiatom, after vacuum dehydroxylation. Diatom samples equilibrated with an 18 O‐enriched δ 18 Oequil. water solution of +94.4‰ at ~21 °C for 70 hr prior to dehydroxylation yield δ 18 Odiatom data that can be directly interpreted with existing empirical δ 18 Odiatom versus temperature relationships. We compare sediment trap‐based δ 18 Odiatom temperature data with modern δ 18 Oforam temperatures. Finally, we present an ~220 year record of δ 18 Odiatom data from an eastern Pacific Guaymas Basin boxcore, analyzed using the microfluorination technique, that indicates diatom chlorophyll maximum (Chlmax ) temperatures have shifted from a period during the late eighteenth and nineteenth centuries that was 8 °C cooler during the fall bloom relative to mean annual alkenone U 37 k ′ sea surface temperature, to the late twentieth century when we observe no difference between alkenone sea surface temperature and diatom Chlmax . These data suggest a twentieth century seasonal shift in the timing of fall upwelling and Guaymas Basin stratification breakdown that could be due to reduced upwelling efficiency and/or increased summer mixed layer thermal stratification. Key Points: Diatom δ 18 O data show predictable alteration at ambient laboratory temperatures due to exchange with rinse water but is correctable Guaymas Basin diatom sediments biased toward the fall bloom and track well with existing foraminifera data sets Diatom δ 18 O temperatures record chlorophyll maximum temperatures warming by ~10°C over a 220 year time frame