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(Table S2) SST estimates as a function of age, ODP Hole 145-887C
This dataset has no description
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(Table S2) SST estimates as a function of age, ODP Site 138-850
Sata from Zhang et al. (2014). -
(Table S2) SST estimates as a function of age, ODP Site 138-846
Alkenone data to 196 mcd Liu andHerbert (2004) and Lawrence, et al. (2006). Data below 196.93 mcd (5.149 Ma)- this work. -
(Table S2) SST estimates as a function of age, DSDP Site 90-594
This dataset has no description
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(Table S3) Age model of ODP Site 162-907C
This dataset has no description
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(Table S3) Age model of ODP Site 162-907B
This dataset has no description
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(Table S3) Age model of ODP Site 201-1225
Ages to 2700 ka follow Cleaveland and Lawrence (in prep.) isotope stratigraphy.Ages to 4200 ka follow Caballero and Herbert (in prep.) isotope stratigraphy.Ages to 4727 Ka... -
(Table S3) Age model of ODP Site 177-1088
This dataset has no description
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(Table S3) Age model of ODP Site 162-982
Ages < 4 Ma derived from Lawrence et al. 2009 partially based on orbital tuning of Lisiecki and Raymo, 2005 of isotopic data from Venz and Hodell, 2002 and Venz et al.,... -
(Table S3) Age model of ODP Hole 151-907A, version A
Ages taken from interpretation of cyrogenic magnetometer data from Initial Reports of the ODP, Leg 151.Bacon parameters: acc.mean=60, acc.shape=3, mem.strength=70, mem.mean=0.49. -
(Table S3) Age model of ODP Site 138-846
Age model to 5.266 Ma follows Lisiecki and Raymo orbital tuning of primary isotope data from Mix et al., 1995.Age model from 5 to 6.2 Ma follows Shackleton et al., 1995. Age... -
(Table S3) Age model of ODP Site 117-722
Age model to 3.35 Ma follows Herbert et al., 2010, which tuned the oxygen isotope record of Clemens et al. 1996 to the LR04 stack.Age control belows approximately follows. Age... -
Sea surface temperature estimates from several sediment cores in the North At...
Here, we have calculated new sea-surface temperature estimates over Dansgaard-Oeschger (DO) events 5-8 (c. 30-40 ka) from 14 sites in the North Atlantic, based on previously... -
Abundance of planktonic Copepoda (Crustacea) during METEOR cruise M42/3 (Grea...
07-11-2018: The identfied specimens of Rhincalanus rostrifrons are probably Rhincalanus cornutus -
(Appendix, pages 275-277) Elemental analysis and manganese oxidizing capacity...
MnOx is determined as 1 + 0.5((2Mn4+ + Mn3+)/(Mn4+ + Mn3+ + Mn2+)).From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal... -
Alkenone concentration and SST reconstruction for ODP Hole 138-846B
Alkenone concentration (this study) and SST (Herbert et al., 2016) data are adapted to the age of our diatom samples (Shackleton et al., 1995). -
Abundance of planktonic Calanoida (Copepoda, Crustacea) from Bongo nets durin...
Only selected calanoid copepods were enumerated. -
(Table S4c) Age control points used for calculation of sedimentation rates of...
This dataset has no description
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(Table S3b) 14C ages measured on Globigerinoides sacculifer of sediment core ...
Jaeschke et al.. 2007; 14C ages from GeoB 3910-2. depths are correlated based on tuned Ti/Ca ratios (see Table S2).14C ages, 14C plateaus, and age conversion into calendar ages... -
(Table S1 b) Definition of planktic 14C plateaus for sediment core GeoB3910-1
Very low sedimentation rates below Plateau 3 suggest hiatus.