FN Archimer Export Format
PT J
TI Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years
BT 
AF UEMURA, Ryu
   MOTOYAMA, Hideaki
   MASSON-DELMOTTE, Valerie
   JOUZEL, Jean
   KAWAMURA, Kenji
   GOTO-AZUMA, Kumiko
   FUJITA, Shuji
   KURAMOTO, Takayuki
   HIRABAYASHI, Motohiro
   MIYAKE, Takayuki
   OHNO, Hiroshi
   FUJITA, Koji
   ABE-OUCHI, Ayako
   IIZUKA, Yoshinori
   HORIKAWA, Shinichiro
   IGARASHI, Makoto
   SUZUKI, Keisuke
   SUZUKI, Toshitaka
   FUJII, Yoshiyuki
AS 1:1;2:2,3;3:4;4:4;5:2,3;6:2,3;7:2,3;8:2;9:2,3;10:2;11:2;12:5;13:6,7;14:8;15:;16:9;17:10;18:11;19:2;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;
C1 Univ Ryukyus, Dept Chem Biol & Marine Sci, 1 Senbaru, Nishihara, Okinawa 9030213, Japan.
   Natl Inst Polar Res, Res Org Informat & Syst, 10-3 Midori Cho, Tachikawa, Tokyo 1908518, Japan.
   Grad Univ Adv Studies SOKENDAI, Dept Polar Sci, 10-3 Midori Cho, Tachikawa, Tokyo 1908518, Japan.
   Univ Paris Saclay, CEA CNRS UVSQ, Inst Pierre Simon Laplace, LSCE,UMR 8212, Gif Sur Yvette, France.
   Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan.
   Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba 2778568, Japan.
   Japan Agcy Marine Earth Sci & Technol, Kanazawa Ku, 3173-25 Showamachi, Yokohama, Kanagawa 2360001, Japan.
   Hokkaido Univ, Inst Low Temp Sci, Kita Ku, North 19 West 8, Sapporo, Hokkaido 0600819, Japan.
   RIKEN, Nishina Ctr, Hirosawa 2-1, Wako, Saitama 3510198, Japan.
   Shinshu Univ, Dept Environm Sci, Asahi 3-1-1, Matsumoto, Nagano 3908621, Japan.
   Yamagata Univ, Dept Earth & Environm Sci, Kojirakawa 1-4-12, Yamagata 9908560, Japan.
C2 UNIV RYUKYUS, JAPAN
   NIPR, JAPAN
   UNIV GRAD ADV STUDIES, JAPAN
   UNIV PARIS SACLAY, FRANCE
   UNIV NAGOYA, JAPAN
   UNIV TOKYO, JAPAN
   JAMSTEC, JAPAN
   UNIV HOKKAIDO, JAPAN
   RIKEN, JAPAN
   UNIV SHINSHU, JAPAN
   UNIV YAMAGATA, JAPAN
IN DOAJ
IF 11.878
TC 41
UR https://archimer.ifremer.fr/doc/00496/60788/64966.pdf
   https://archimer.ifremer.fr/doc/00496/60788/64967.pdf
LA English
DT Article
CR MD 125 / SWIFT BIS-CARHOT
   NAUSICAA-IMAGES 2-MD105
   VT 90 / SOUC
BO Marion Dufresne
AB The delta D temperature proxy in Antarctic ice cores varies in parallel with CO2 through glacial cycles. However, these variables display a puzzling asynchrony. Well-dated records of Southern Ocean temperature will provide crucial information because the Southern Ocean is likely key in regulating CO2 variations. Here, we perform multiple isotopic analyses on an Antarctic ice core and estimate temperature variations at this site and in the oceanic moisture source over the past 720,000 years, which extend the longest records by 300,000 years. Antarctic temperature is affected by large variations in local insolation that are induced by obliquity. At the obliquity periodicity, the Antarctic and ocean temperatures lag annual mean insolation. Further, the magnitude of the phase lag is minimal during low eccentricity periods, suggesting that secular changes in the global carbon cycle and the ocean circulation modulate the phase relationship among temperatures, CO2 and insolation in the obliquity frequency band. 
PY 2018
PD MAR
SO Nature Communications
SN 2041-1723
PU Nature Publishing Group
VL 9
IS 961
UT 000426659300007
DI 10.1038/s41467-018-03328-3
ID 60788
ER

EF