MODERN AND PLEISTOCENE RESERVOIR AGES INFERRED FROM SOUTH PACIFIC CORALS

被引:29
作者
Burr, G. S. [1 ,2 ]
Beck, J. W. [1 ]
Correge, Thierry [3 ]
Cabioch, G. [4 ]
Taylor, F. W. [5 ]
Donahue, D. J. [1 ]
机构
[1] Univ Arizona, Dept Phys, NSF Arizona AMS Lab, Tucson, AZ 85721 USA
[2] Natl Taiwan Univ, Dept Geosci, Taipei 10764, Taiwan
[3] Univ Bordeaux 1, F-33405 Talence, France
[4] Ctr Ile France, IRD, UMR LOCEAN, F-93143 Bondy, France
[5] Univ Texas Austin, Inst Geophys, Austin, TX 78758 USA
基金
美国国家科学基金会;
关键词
SURFACE OCEAN RADIOCARBON; PAPUA-NEW-GUINEA; CARBON-DIOXIDE EXCHANGE; CAL KYR BP; SOUTHWESTERN PACIFIC; BOMB RADIOCARBON; MARINE SAMPLES; YOUNGER DRYAS; C-14; RECORD; TH-230; AGES;
D O I
10.1017/S0033822200033853
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper presents radiocarbon results from modern South Pacific corals from the Marquesas Islands, Vanuatu. Papua New Guinea (PNG), and Easter Island. All of the measurements are from pre-bomb Porites corals that lived during the 1940s and 1950s. The data reflect subannual to multiannual surface ocean C-14 variability and allow for precise. unambiguous reservoir age determinations. The results are compared with published values from other coral records throughout the South Pacific, with striking consistency. By comparisons with other published values, we identify 3 South Pacific regions with uniform pre-bomb reservoir ages (1945 to 1955). These are I) the Central Equatorial South Pacific (361.6 +/- 8.2 C-14 yr. 2 sigma); 2) the Western Equatorial South Pacific (322.1 +/- 8.6 C-14 yr, 2 sigma): and 3) the subtropical Pacific (266.8 +/- 13.8 C-14 yr, 2 sigma). The question of how much, and how fast, South Pacific reservoir ages might have varied in the past is addressed by examining a published record from a Pleistocene coral from Vanuatu that lived over a 700-yr period during the Younger Dryas. The average reservoir age at that time was larger than today, by similar to 150 yr, and exhibited reservoir age variability on a decadal timescale not seen in modern times. Measured paleo-reservoir ages increase sharply in this record by as many as 300 C-14 yr in 3 decades. These increases are punctuated by smaller reservoir age decreases, on the order of 150 yr. This reservoir age variability provides a rare picture of active ocean ventilation and ocean-atmosphere exchange at the close of the Pleistocene.
引用
收藏
页码:319 / 335
页数:17
相关论文
共 52 条
[1]  
Bonjean F, 2002, J PHYS OCEANOGR, V32, P2938, DOI 10.1175/1520-0485(2002)032<2938:DMAAOT>2.0.CO
[2]  
2
[3]   INTRAANNUAL VARIABILITY OF THE RADIOCARBON CONTENT OF CORALS FROM THE GALAPAGOS-ISLANDS [J].
BROWN, TA ;
FARWELL, GW ;
GROOTES, PM ;
SCHMIDT, FH ;
STUIVER, M .
RADIOCARBON, 1993, 35 (02) :245-251
[4]   A high-resolution radiocarbon calibration between 11,700 and 12,400 calendar years BP derived from 230Th ages of corals from Espiritu Santo Island, Vanuatu [J].
Burr, GS ;
Beck, JW ;
Taylor, FW ;
Récy, J ;
Edwards, RL ;
Cabioch, G ;
Corrége, T ;
Donahue, DJ ;
O'Malley, JM .
RADIOCARBON, 1998, 40 (03) :1093-1105
[5]   Radiocarbon results from a 13-kyr BP coral from the Huon Peninsula, Papua New Guinea [J].
Burr, GS ;
Galang, C ;
Taylor, FW ;
Gallup, C ;
Edwards, RL ;
Cutler, K ;
Quirk, B .
RADIOCARBON, 2004, 46 (03) :1211-1224
[6]   The half-lives of uranium-234 and thorium-230 [J].
Cheng, H ;
Edwards, RL ;
Hoff, J ;
Gallup, CD ;
Richards, DA ;
Asmerom, Y .
CHEMICAL GEOLOGY, 2000, 169 (1-2) :17-33
[7]   Interdecadal variation in the extent of South Pacific tropical waters during the Younger Dryas event [J].
Corrège, T ;
Gagan, MK ;
Beck, JW ;
Burr, GS ;
Cabioch, G ;
Le Cornec, F .
NATURE, 2004, 428 (6986) :927-929
[9]   THE NATURAL DISTRIBUTION OF RADIOCARBON AND THE EXCHANGE TIME OF CARBON DIOXIDE BETWEEN ATMOSPHERE AND SEA [J].
CRAIG, H .
TELLUS, 1957, 9 (01) :1-17
[10]   Radiocarbon calibration and comparison to 50 kyr BP with paired 14C and 230Th dating of corals from Vanuatu and Papua New Guinea [J].
Cutler, KB ;
Gray, SC ;
Burr, GS ;
Edwards, RL ;
Taylor, FW ;
Cabioch, G ;
Beck, JW ;
Cheng, H ;
Moore, J .
RADIOCARBON, 2004, 46 (03) :1127-1160