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Stern, Joseph V; Lisiecki, Lorraine E (2018): Regional benthic δ¹⁸O stacks and their δ¹⁸O uncertainties [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.891137, Supplement to: Stern, JV; Lisiecki, LE (2014): Termination 1 timing in radiocarbon-dated regional benthic δ18O stacks. Paleoceanography, 29(12), 1127-1142, https://doi.org/10.1002/2014PA002700

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Abstract:
Benthic δ18O changes are often assumed to be globally synchronous, but studies comparing 2–9 radiocarbon‐dated records over the most recent deglaciation (Termination 1) have proposed differences in the timing of benthic δ18O change between the Atlantic and Pacific, intermediate and deep, and North and South Atlantic. Because of the relatively small number of records used in these previous studies, it has remained unclear whether these differences are local or regional in scale. Here we present seven regional benthic δ18O stacks for 0–40 kyr B.P. that include 252 records with independent regional age models constrained by 852 planktonic foraminiferal 14C dates from 61 of these cores. We find a 4000 year difference between the earliest termination onset in the intermediate South Atlantic at 18.5 (95% confidence interval: 17.9–19.0) kyr B.P. and the latest in the deep Indian at 14.5 (14.1–15.0) kyr B.P. The termination onset occurs at 17.5 kyr B.P. in the intermediate and deep North Atlantic, deep South Atlantic, and deep Pacific. However, throughout the termination deep North Atlantic benthic δ18O leads the deep Pacific by an average of 1000 year and a maximum of 1700 year. Additionally, the intermediate Pacific termination onset at 16.5 (16.1–16.9) kyr B.P. demonstrates that intermediate‐depth benthic δ18O change was not globally synchronous. These regional stacks provide better age models than a global stack across Termination 1 and potentially important constraints on deglacial ocean circulation changes.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPStern, Joseph VGeocode
2δ18Oδ18OStern, Joseph VIntermediate North Atlantic stack
3Number of pointsPoints#Stern, Joseph VIntermediate North Atlantic, number of points in stacked interval
4δ18O, standard errorδ18O std e±Stern, Joseph VIntermediate North Atlantic, standard error for stacked d18O
5δ18Oδ18OStern, Joseph VDeep North Atlantic stack
6Number of pointsPoints#Stern, Joseph VDeep North Atlantic, number of points in stacked interval
7δ18O, standard errorδ18O std e±Stern, Joseph VDeep North Atlantic, standard error for stacked d18O
8δ18Oδ18OStern, Joseph VIntermediate South Atlantic stack
9Number of pointsPoints#Stern, Joseph VIntermediate South Atlantic, number of points in stacked interval
10δ18O, standard errorδ18O std e±Stern, Joseph VIntermediate South Atlantic, standard error for stacked d18O
11δ18Oδ18OStern, Joseph VDeep South Atlantic stack
12Number of pointsPoints#Stern, Joseph VDeep South Atlantic, number of points in stacked interval
13δ18O, standard errorδ18O std e±Stern, Joseph VDeep South Atlantic, standard error for stacked d18O
14δ18Oδ18OStern, Joseph VIntermediate Pacific stack
15Number of pointsPoints#Stern, Joseph VIntermediate Pacific, number of points in stacked interval
16δ18O, standard errorδ18O std e±Stern, Joseph VIntermediate Pacific, standard error for stacked d18O
17δ18Oδ18OStern, Joseph VDeep Pacific stack
18Number of pointsPoints#Stern, Joseph VDeep Pacific, number of points in stacked interval
19δ18O, standard errorδ18O std e±Stern, Joseph VDeep Pacific, standard error for stacked d18O
20δ18Oδ18OStern, Joseph VDeep Indian stack
21Number of pointsPoints#Stern, Joseph VDeep Indian, number of points in stacked interval
22δ18O, standard errorδ18O std e±Stern, Joseph VDeep Indian, standard error for stacked d18O
Size:
1794 data points

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