A Ternary Mixing Model Approach Using Benthic Foraminifer δ13C‐δ18O Data to Reconstruct Late Pliocene Deep Atlantic Water Mass Mixing. Issue 12 (2nd December 2020)

• Record Type: Journal Article
• Authors: van der Weijst, Carolien M. H.; Winkelhorst, Josse; Lourens, Lucas; Raymo, Maureen E.; Sangiorgi, Francesca; Sluijs, Appy
• Is Part Of: Paleoceanography and paleoclimatology. Volume 35:Issue 12(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-12-02
• Subjects: Pliocene -- Atlantic Meridional Overturning Circulation -- benthic δ13C‐δ18O -- ternary mixing model -- M2 glacial -- eastern equatorial Atlantic; Paleoceanography -- Periodicals; Paleoclimatology -- Periodicals; 551.46
• DOI: 10.1029/2019PA003804
• Languages: English
• ISSNs: 2572-4517

Abstract

Abstract: Late Pliocene deep Atlantic δ 13 C data have been interpreted as evidence for enhanced Atlantic Meridional Overturning Circulation (AMOC) compared to the present, but this hypothesis is not supported by the Pliocene Model Intercomparison Project (PlioMIP). Here, we adopt a new approach to assess variability in deep ocean circulation based on paired stable carbon (δ 13 C) and oxygen isotopes (δ 18 O) of benthic foraminifera, both (semi)conservative water mass tracers. Assuming that deep Atlantic benthic δ 13 C‐δ 18 O variability is predominantly driven by mixing, we extrapolate the δ 13 C‐δ 18 O data outside the sampled range to identify the end‐members. At least three end‐members are needed to explain the spatial δ 13 C‐δ 18 O variability in the deep North Atlantic Ocean: two Northern Component Water (NCW) and one Southern Component Water (SCW) water masses. We use a ternary mixing model to quantify the mixing proportions between SCW and NCW in the deep Atlantic Ocean. Our analysis includes new data from Ocean Drilling Program Sites 959 and 662 in the eastern equatorial Atlantic and suggests that the AMOC cell was deeper during the M2 glacial than during late Pliocene interglacials. Moreover, we identify a new cold and well‐ventilated water mass that was geographically restricted to the southeast Atlantic Ocean between 3.6 and 2.7 Ma and did not contribute significantly to the δ 13 C‐δ 18 O variability of the rest of the basin. This high‐δ 13 C high‐δ 18 O water mass has led to the misconception of a reduced latitudinal δ 13 C gradient. Our analyses show that the late Pliocene δ 13 C gradient between NCW and SCW was similar to the present‐day value of 1.1‰. Key Points: Paired δ 13 C‐δ 18 O data are used to identify water mass end‐members outside the sampled range In past oceans, a ternary mixing model using δ 13 C‐δ 18 O may outperform a binary δ 13 C mixing model AMOC was relatively deep during the M2 glacial compared to the late Pliocene interglacials