Li et al. (1989)Li WX, Lundberg J, Dickin AP, Ford DC, Schwarcz HP, Mcnutt R and Williams D. 1989. High-precision mass-spectrometric uranium-series dating of cave deposits and implications for palaeoclimate studies. Nature 339: 534-536.
|
Bahamas |
220-212 |
7c |
>-10 to -15 |
235-230 |
7e |
Pirazzoli et al. (1991)Pirazzoli PA, Radtke U, Hantoro WS, Jouannic C, Hoang CT, Causse C and Best MB. 1991. Quaternary raised coral-reef terraces on Sumba Island, Indonesia. Science 252: 1834-1836.
|
Indonesia |
232 ± 35 |
7e |
-12 ± 12 |
Gallup et al. (1994)Gallup CD, Edwards RL and Johnson RG. 1994. The timing of high sea levels over the past 200,000 years. Science 263: 796-800.
|
Barbados |
201-193 |
7a |
-6 to +9 |
Hearty and Kindler (1995)Hearty OJ and Kindler P. 1995. Sea level highstand chronology from stable carbonate platforms (Bermuda and the Bahamas). J Coastal Res 11(3): 675-689.
|
Bahamas, Bermuda |
240-230 |
7e |
≤ 0 |
Bermuda |
210-180 |
7a |
+2.5 |
Roy et al. (1997)Roy PS, Zhuang W-Y, Birch GF, Cowell PJ and Li C. 1997. Quaternary geology of the Forster-Tuncurry coast and shelf, southeast Australia. Geological Survey of New South Wales, 405 p.
|
Australia |
261-217 |
7a-c |
+2 to +4 |
Vesica et al. (2000)Vesica PL, Tuccimei P, Turi B, Fornós JJ, Ginés A and Ginés J. 2000. Late Pleistocene Paleoclimates and sea level change in the Mediterranean as inferred from stable isotope and U-series studies of overgrowths on speleothems, Mallorca, Spain. Quaternary Sci Rev 19: 865-879.
|
Spain |
231 ± 28 |
7e |
+4.2 |
Bard et al. (2002)Bard E, Antonioli F and Silenzi S. 2002. Sea level during the penultimate interglacial period based on a submerged stalagmite from Argentarola Cave (Italy). Earth Planet Sc Lett 196: 135-146.
|
Italy |
202-190 |
7a |
-18.5 to -9 |
Barreto et al. (2002)Barreto AMF, Bezerra FHR, Suguio K, Tatumi SH, Yee M, Paiva RP and Munita CS. 2002. Late Pleistocene marine terrace deposits in northeastern Brazil: sea level change and tectonic implications. Palaeogeogr Palaeocl Paleoecol 179: 57-69.
|
NE Brazil |
207 ± 4 |
7c |
+3 to +5 |
220 ± 2 |
Robinson et al. (2002)Robinson LF, Henderson GM and Slowey NC. 2002. U-Th dating of marine isotope stage 7 in Bahamas slope sediments. Earth Planet Sci Lett 196: 175-187.
|
Bahamas |
235 |
7e |
-5 |
Murray-Wallace (2002)Murray-Wallace CV. 2002. Pleistocene coastal stratigraphy, sea level highstands and neotectonism of the southern Australian passive margin – a review. J Quaternary Sci 17(5-6): 469-489.
|
Australia |
230 ± 11 |
7e |
-6.0
|
258 ± 11 |
7e |
0.0
|
Waelbroeck et al. (2002)Waelbroeck C, Labeyrie L, Michel E, Duplessy JC, Mcmanus JF, Lambeck K, Balbon E and Labracherie M. 2002. Sea level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Sci Rev 21: 295-305.
|
N. Atlantic / Eq. Pacific |
240-235 |
7e |
-10 |
∼220 |
7c |
∼ -5 |
∼195 |
7a |
∼ -10 |
Lea et al. (2002)Lea DW, Martin PA, Pak DK and Spero HJ. 2002. Reconstructing a 350 ky history of sea level using planktonic Mg/Ca and oxygen isotope records from a Cocos Ridge core. Quaternary Sci Rev 21: 283-293.
|
Pacific |
∼240 |
7e |
∼0 |
∼215 |
7c |
∼ -10 |
∼200 |
7a |
∼0 |
Schellmann and Radtke (2004)Schellmann G and Radtke U. 2004. A revised morpho- and chronostratigraphy of the Late and Middle Pleistocene coral reef terraces on Southern Barbados (West Indies). Earth-Sci Rev 64: 157-187.
|
Barbados |
222 |
7a |
-16.0 |
224 |
7c |
-3.0 |
Goy et al. (2006) |
Spain |
237 ± 20 |
7e |
-1 |
Dutton et al. (2009)Dutton A, Bard E, Antonioli F, Esat TM, Lambeck K and McCulloch T. 2009. Phasing and amplitude of sea level and climate change during the penultimate interglacial. Nate Geosci 2: 355-359.
|
Italy |
201.5 ± 1.7 to 189.7 ± 1.5 |
7a |
-18 |
217.2 ± 1.9 to 206.0 ± 1.9 |
7c |
248.9 ± 19 to 231.0 ± 3.0 |
7e |
Suguio et al. (2011)Suguio K, Bezerra FHR and Barreto AMF. 2011. Luminescence dated Late Pleistocene wave-built terraces in northeastern Brazil. An Acad Bras Cienc 83(3): 907-920.
|
NE Brazil |
212 ± 4 |
7c |
>+1.7 |
220 ± 22 |
7c |
>+4 |
This paper |
S Brazil |
∼230 |
7e |
∼ +10 ± 1 |