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  • 1
    Publication Date: 2024-03-02
    Keywords: 06MT15_2; 108-658A; 117-723; 117-728A; 130-806B; 133-820; 145-882; 146-893A; 160-967C; 160-971A; 161-975; 161-976; 161-977A; 165-1002C; 165-999A; 167-1012; 167-1014; 167-1016; 167-1017B; 167-1018A; 167-1019C; 167-1020; 177-1090; 177-1094; 181-1123; 184-1144A; 184-1145; 202-1239; 90-593_Site; 90-594_Site; A150/180; A180-73; Agulhas Basin; Agulhas Ridge; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; Angola Basin; ANT-IX/4; ANT-VIII/3; ANT-XI/2; ANT-XXVI/2; APSARA4; Arabian Sea; Arctic Ocean; ARK-II/5; Atlantic Ocean; Australia; Azores; Bermuda Rise; Bicol shelf; BIGSET; BIO; Biology; Brazil Basin; C9001C; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso Square Core System; Canarias Sea; Caribbean Sea; CASQS; Cayman Rise, Caribbean Sea; CH69-K09; Change-Le_CL01; Chatham Rise; Cocos Ridge; COMPCORE; Composite Core; Congo Fan; Coral Sea; Core; CORE; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Basin; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Equatorial Atlantic; Equatorial East Pacific; Event label; EW03; EW9302; EW9302-JPC8; FR1/94-GC3; GC; GeoB10038-4; GeoB1008-3; GeoB1016-3; GeoB1028-5; GeoB1105-4; GeoB1112-4; GeoB1309-2; GeoB1312-2; GeoB1401-4; GeoB1523-1; GeoB1710-3; GeoB1711; GeoB1711-4; GeoB1712-4; GeoB1722-1; GeoB2204-2; GeoB3005-1; GeoB3603-2; GEOSCIENCES, MARMARCORE; Giant piston corer; GIK12392-1; GIK15637-1; GIK17732-1; GIK17954-2; GIK17961-2; GIK23243-1 PS05/431; GIK23323-1; GIK23352-3; GIK23414-5; GL-77; global reconstruction; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); GS900963; Gulf of California; Hainan_Island-S009; Huon_Peninsula; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES VIII - MONA; IMAGES VII - WEPAMA; IMAGES XII - MARCO POLO; IMAGES XI - P.I.C.A.S.S.O.; IMAGES XIV - MARCO POLO 2; Indian Ocean; Japan Trench; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KAL; KALMAR II; Kasten corer; KH94-4TSP-2PC; KL; KOL; KS205; Last Interglacial; LATITUDE; Leg108; Leg117; Leg130; Leg133; Leg145; Leg146; Leg160; Leg161; Leg165; Leg167; Leg177; Leg181; Leg184; Leg202; Leg90; Le Suroît; LONGITUDE; LPAZ-21P; M12392-1; M13/2; M15/2; M16/1; M16/2; M17/2; M20/2; M23/3; M23414; M25; M31/3; M31/3-108_GC; M34/1; M35/1; M35027-1; M53; M6/6; M7/4; M7/5; M9/4; Marge Ibérique; Marion Dufresne (1972); Marion Dufresne (1995); MATACORE; Maurice Ewing; MD00; MD012378; MD01-2378; MD012421; MD01-2421; MD01-2444/2443; MD022529; MD02-2529; MD02-2594; MD032616; MD03-2616; MD032664; MD03-2664; MD03-2707; MD052896; MD05-2896; MD052904; MD05-2904; MD062986; MD06-2986; MD06-3052; MD101; MD106; MD111; MD122; MD123; MD126; MD128; MD132; MD147; MD152; MD155; MD65; MD73025-2; MD85668; MD85674; MD88-770; MD90-963; MD952036; MD95-2036; MD952037; MD95-2037; MD952040; MD95-2040; MD952042; MD95-2042; MD972106; MD97-2106; MD972108; MD97-2108; MD972120; MD97-2120; MD972121; MD97-2121; MD972125; MD97-2125; MD972142; MD97-2142; MD972151; MD97-2151; MD982162; MD98-2162; Mediterranean Sea; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; Namibia continental slope; Newfoundland margin; NingalooReef; North Atlantic; Northeast Atlantic; North Pacific Ocean; Northwestern Pacific Ocean; Norwegian Sea; Number of points; OSIRIS I; P-013; P71; PABESIA; PALEOCINAT; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS05; PS1243-1; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-3; PS2489-2; PS28; PS28/256; PS75/034-2; PS75 BIPOMAC; RC08; RC08-145; RC08-39; RC10; RC10-62; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-110; RC13-115; RC13-205; RC13-228; RC13-229; RC14; RC14-105; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature; Sea surface temperature, annual mean; Sea surface temperature, annual mean, standard deviation; Sea Surface Temperatures; SEYMAMA/SHIVA; Shirshov Ridge; Site; SK157/4; SL; SO136; SO136_003GC; SO184/1; SO201/2; SO201-2-85; SO95; Sonne; South Atlantic Ocean; South China Sea; South-East Pacific; Southern Cape Basin; Southern Ocean; South Pacific; South Pacific/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; South Tasman Rise; Southwest Pacific Ocean; SST; SU90-08; SU94-20bK; Super-interglacial; SWAF; TASQWA; Temperature anomaly; Temperature anomaly, standard deviation; TG7; Thermoluminescence, standard deviation; Thomas Washington; Timor Sea; TR126-23; TR126-29; TR163-19; TR163-22; TY93929/P; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; VNTR01; VNTR01-8PC; W8402A; W8402A-14; Walvis Ridge, Southeast Atlantic Ocean; Wecoma; Western Arabian See; Western Basin; Y69-106P; Y69-71P; Y71-06; Y71-06-12; Y71-09; Y71-09-101; Y71-3-2; Y7211; Y7211-1; Y9; Y9_core; YALOC69; Yaquina; Z14-16; Z2108
    Type: Dataset
    Format: text/tab-separated-values, 2262 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-02-29
    Keywords: 145-882; 167-1019C; 167-1020; 177-1090; 177-1094; 181-1123; 90-593_Site; Agulhas Basin; Agulhas Ridge; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; ANT-XI/2; ANT-XXVI/2; APSARA4; C9001C; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; CH69-K09; Chatham Rise; COMPCORE; Composite Core; Core; CORE; D117; DRILL; Drilling/drill rig; E45-29; E49-18; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; FR1/94-GC3; GC; GIK23414-5; global reconstruction; Glomar Challenger; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KALMAR II; KL; Last Interglacial; LATITUDE; Leg145; Leg167; Leg177; Leg181; Leg90; LONGITUDE; M17/2; M23414; Marion Dufresne (1972); Marion Dufresne (1995); MATACORE; Maurice Ewing; MD00; MD032664; MD03-2664; MD062986; MD06-2986; MD101; MD106; MD132; MD152; MD73025-2; MD88-770; MD952040; MD95-2040; MD972106; MD97-2106; MD972108; MD97-2108; MD972120; MD97-2120; Meteor (1986); Meteor Rise; Method comment; MUC; MultiCorer; Newfoundland margin; North Pacific Ocean; Northwestern Pacific Ocean; Norwegian Sea; Number of points; OSIRIS I; P-013; PC; Piston corer; Piston corer (BGR type); Polarstern; Porto Seamount; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-1; PS2489-2; PS28; PS28/256; PS75/034-2; PS75 BIPOMAC; RC08; RC08-39; RC11; RC1112; RC11-120; RC15; RC15-61; Reference/source; Robert Conrad; Sea surface temperature, annual mean; Sea Surface Temperatures; Shirshov Ridge; Site; SL; SO136; SO136_003GC; SO201/2; SO201-2-85; Sonne; South Atlantic Ocean; South Pacific; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; South Tasman Rise; Southwest Pacific Ocean; SST; SU90/08; Super-interglacial; Tasman Sea; TASQWA; Temperature, difference; TSP-2PC; V18; V18-68; V20; V20-120; V22; V22-108; V23; V23-82; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-14; V28-56; V29; V29-179; V30; V30-97; Vema; Y7211; Y7211-1; Y9; Y9_core; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 378 data points
    Location Call Number Expected Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Turney, Chris S M; Jones, Richard; McKay, Nicholas; Van Sebille, Erik; Thomas, Zoë Amber; Hillenbrand, Claus-Dieter; Fogwill, Chris J (in review): A global mean sea-surface temperature dataset for the Last Interglacial (129–116 kyr) and contribution of thermal expansion to sea-level change. Earth System Science Data Discussions, https://doi.org/10.5194/essd-2019-249
    Publication Date: 2024-02-26
    Description: A valuable analogue for assessing Earth's sensitivity to warming is the Last Interglacial (LIG; 129-116 kyr), when global temperatures and mean sea level were higher than today. We report here a global network of LIG sea-surface temperatures (SST) obtained from various published temperature proxies (e.g. faunal/floral plankton assemblages, Mg/Ca ratios of calcareous organisms, and alkenone UK'37). Each reconstruction is averaged across the LIG (anomalies relative to 1981-2010), corrected for ocean drift and with varying seasonality (189 annual, 99 December-February, and 92 June-August). Because of local δ18O seawater changes, uncertainty in the age models of marine cores, and differences in sampling resolution and/or sedimentation rates, we do not attempt to resolve changes within the LIG. Therefore, and to avoid bias towards individual LIG SSTs based on only a single (and potentially erroneous) measurement or a single interpolated data point, we report temperatures averaged across the entire LIG. The global dataset provides a remarkably coherent pattern of higher SST increases at polar latitudes than in the tropics, with comparable estimates between different SST proxies.
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
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  • 4
    Publication Date: 2024-02-29
    Keywords: 06MT15_2; 108-658A; 161-975; 161-976; 162-980; A150/180; A180-73; Agulhas Basin; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; Atlantic Ocean; Brazil Basin; CALYPSO; Calypso Corer; Canarias Sea; CH69-K09; Charles Darwin; COMPCORE; Composite Core; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; GC; GeoB1309-2; GeoB1312-2; GeoB1523-1; GeoB2204-2; GIK12392-1; GIK15637-1; GIK17954-2; GIK23323-1; GIK23414-5; GL-77; global reconstruction; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES II; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; JPC37; Jumbo Piston Core; K708-001; K708-007; KAL; KAL15; Kasten corer; Kasten corer 15 cm; KL; KOL; Last Interglacial; LATITUDE; Leg108; Leg161; Leg162; Le Suroît; LONGITUDE; M12392-1; M15/2; M16/2; M17/2; M23/3; M23414; M25; M35/1; M35027-1; M53; M7/4; Marion Dufresne (1972); Marion Dufresne (1995); Maurice Ewing; MD00; MD032664; MD03-2664; MD101; MD105; MD106; MD132; MD73025-2; MD952040; MD95-2040; MD962085; MD96-2085; MD972142; MD97-2142; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; NA87-25; NEAP; NEAP-18K; Newfoundland margin; North Atlantic; Northeast Atlantic; Norwegian Sea; Number of points; off Orange River; OSIRIS I; P-013; PALEOCINAT; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-3; RC08; RC08-145; RC08-39; RC10; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-205; RC13-228; RC13-229; RC14; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature, June-August; Sea surface temperature, June-August, standard deviation; Sea Surface Temperatures; Site; SL; SO95; Sonne; South Atlantic Ocean; South China Sea; SST; SU90-03; Super-interglacial; TR126-23; TR126-29; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; Western Basin; Y71-06; Y71-06-12; Y7211; Y7211-1; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 1104 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-03-02
    Keywords: 06MT15_2; 108-658A; 117-723; 117-728A; 130-806B; 133-820; 145-882; 146-893A; 160-967C; 160-971A; 161-975; 161-976; 161-977A; 165-1002C; 165-999A; 167-1012; 167-1014; 167-1016; 167-1017B; 167-1018A; 167-1019C; 167-1020; 177-1090; 177-1094; 181-1123; 184-1144A; 184-1145; 202-1239; 90-593_Site; 90-594_Site; A150/180; A180-73; Agulhas Basin; Agulhas Ridge; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; Angola Basin; ANT-IX/4; ANT-VIII/3; ANT-XI/2; ANT-XXVI/2; APSARA4; Arabian Sea; Arctic Ocean; ARK-II/5; Atlantic Ocean; Australia; Azores; Bermuda Rise; Bicol shelf; BIGSET; BIO; Biology; Brazil Basin; C9001C; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso Square Core System; Canarias Sea; Caribbean Sea; CASQS; Cayman Rise, Caribbean Sea; CH69-K09; Change-Le_CL01; Chatham Rise; Cocos Ridge; COMPCORE; Composite Core; Congo Fan; Coral Sea; Core; CORE; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Basin; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Equatorial Atlantic; Equatorial East Pacific; Event label; EW03; EW9302; EW9302-JPC8; FR1/94-GC3; GC; GeoB10038-4; GeoB1008-3; GeoB1016-3; GeoB1028-5; GeoB1105-4; GeoB1112-4; GeoB1309-2; GeoB1312-2; GeoB1401-4; GeoB1523-1; GeoB1710-3; GeoB1711; GeoB1711-4; GeoB1712-4; GeoB1722-1; GeoB2204-2; GeoB3005-1; GeoB3603-2; GEOSCIENCES, MARMARCORE; Giant piston corer; GIK12392-1; GIK15637-1; GIK17732-1; GIK17954-2; GIK17961-2; GIK23243-1 PS05/431; GIK23323-1; GIK23352-3; GIK23414-5; GL-77; global reconstruction; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); GS900963; Gulf of California; Hainan_Island-S009; Huon_Peninsula; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES VIII - MONA; IMAGES VII - WEPAMA; IMAGES XII - MARCO POLO; IMAGES XI - P.I.C.A.S.S.O.; IMAGES XIV - MARCO POLO 2; Indian Ocean; Japan Trench; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KAL; KALMAR II; Kasten corer; KH94-4TSP-2PC; KL; KOL; KS205; Last Interglacial; LATITUDE; Leg108; Leg117; Leg130; Leg133; Leg145; Leg146; Leg160; Leg161; Leg165; Leg167; Leg177; Leg181; Leg184; Leg202; Leg90; Le Suroît; LONGITUDE; LPAZ-21P; M12392-1; M13/2; M15/2; M16/1; M16/2; M17/2; M20/2; M23/3; M23414; M25; M31/3; M31/3-108_GC; M34/1; M35/1; M35027-1; M53; M6/6; M7/4; M7/5; M9/4; Marge Ibérique; Marion Dufresne (1972); Marion Dufresne (1995); MATACORE; Maurice Ewing; MD00; MD012378; MD01-2378; MD012421; MD01-2421; MD01-2444/2443; MD022529; MD02-2529; MD02-2594; MD032616; MD03-2616; MD032664; MD03-2664; MD03-2707; MD052896; MD05-2896; MD052904; MD05-2904; MD062986; MD06-2986; MD06-3052; MD101; MD106; MD111; MD122; MD123; MD126; MD128; MD132; MD147; MD152; MD155; MD65; MD73025-2; MD85668; MD85674; MD88-770; MD90-963; MD952036; MD95-2036; MD952037; MD95-2037; MD952040; MD95-2040; MD952042; MD95-2042; MD972106; MD97-2106; MD972108; MD97-2108; MD972120; MD97-2120; MD972121; MD97-2121; MD972125; MD97-2125; MD972142; MD97-2142; MD972151; MD97-2151; MD982162; MD98-2162; Mediterranean Sea; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; Namibia continental slope; Newfoundland margin; NingalooReef; North Atlantic; Northeast Atlantic; North Pacific Ocean; Northwestern Pacific Ocean; Norwegian Sea; OSIRIS I; P-013; P71; PABESIA; PALEOCINAT; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS05; PS1243-1; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-3; PS2489-2; PS28; PS28/256; PS75/034-2; PS75 BIPOMAC; RC08; RC08-145; RC08-39; RC10; RC10-62; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-110; RC13-115; RC13-205; RC13-228; RC13-229; RC14; RC14-105; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature; Sea surface temperature, annual mean; Sea surface temperature, annual mean, standard deviation; Sea Surface Temperatures; SEYMAMA/SHIVA; Shirshov Ridge; Site; SK157/4; SL; SO136; SO136_003GC; SO184/1; SO201/2; SO201-2-85; SO95; Sonne; South Atlantic Ocean; South China Sea; South-East Pacific; Southern Cape Basin; Southern Ocean; South Pacific; South Pacific/CONT RISE; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; South Tasman Rise; Southwest Pacific Ocean; SST; SU90-08; SU94-20bK; Super-interglacial; SWAF; TASQWA; Temperature anomaly; Temperature anomaly, standard deviation; TG7; Thermoluminescence, standard deviation; Thomas Washington; Timor Sea; TR126-23; TR126-29; TR163-19; TR163-22; TY93929/P; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; VNTR01; VNTR01-8PC; W8402A; W8402A-14; Walvis Ridge, Southeast Atlantic Ocean; Wecoma; Western Arabian See; Western Basin; Y69-106P; Y69-71P; Y71-06; Y71-06-12; Y71-09; Y71-09-101; Y71-3-2; Y7211; Y7211-1; Y9; Y9_core; YALOC69; Yaquina; Z14-16; Z2108
    Type: Dataset
    Format: text/tab-separated-values, 2073 data points
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2024-03-02
    Keywords: 06MT15_2; 108-658A; 161-976; 177-1089; 177-1094; A150/180; A180-73; Agulhas Basin; Agulhas Ridge; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; ANT-X/5; ANT-XI/2; ANT-XI/4; ANT-XVIII/5a; APSARA2; Atlantic Ridge; Brazil Basin; CALYPSO; Calypso Corer; Canarias Sea; CH69-K09; COMPCORE; Composite Core; Cosmonauts Sea; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; GC; GeoB1309-2; GeoB1312-2; GeoB1523-1; GeoB2204-2; GIK12392-1; GIK15637-1; GIK17954-2; GIK23414-5; GL-77; global reconstruction; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KAL; Kasten corer; KL; KOL; Last Interglacial; LATITUDE; Leg108; Leg161; Leg177; LONGITUDE; M12392-1; M15/2; M16/2; M17/2; M23/3; M23414; M25; M35/1; M35027-1; M53; Marion Dufresne (1972); Marion Dufresne (1995); Maurice Ewing; MD00; MD032664; MD03-2664; MD101; MD106; MD132; MD38; MD73025-2; MD84-527; MD84-551; MD952040; MD95-2040; MD972142; MD97-2142; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; Newfoundland margin; Northeast Atlantic; Norwegian Sea; Number of points; OSIRIS I; P-013; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS16; PS16/271; PS16/278; PS16/311; PS16/345; PS1752-1; PS1754-1; PS1768-8; PS1778-5; PS18; PS18/232; PS18/238; PS18/260; PS2076-3; PS2082-1; PS2102-2; PS22/769; PS22/803; PS22 06AQANTX_5; PS2276-4; PS2305-6; PS2489-2; PS2603-3; PS28; PS28/256; PS30; PS30/140; PS58; PS58/271-1; RC08; RC08-145; RC08-39; RC10; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-205; RC13-228; RC13-229; RC14; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature, December-February; Sea surface temperature, December-February, standard deviation; Sea Surface Temperatures; Shona Ridge; Site; SL; SO95; Sonne; South Atlantic Ocean; South China Sea; Southeast Pacific; South Indian Ocean; SST; Super-interglacial; TR126-23; TR126-29; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; Y71-06; Y71-06-12; Y7211; Y7211-1; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 1188 data points
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  • 7
    Publication Date: 2019-10-10
    Print ISSN: 0722-4060
    Electronic ISSN: 1432-2056
    Topics: Biology
    Published by Springer
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  • 8
    Publication Date: 2019-06-10
    Description: Precise radiocarbon (14C) dating of sedimentary sequences is important for developing robust chronologies of environmental change, but sampling of suitable components can be challenging in highly dynamic landscapes. Here we investigate radiocarbon determinations of different peat size fractions from six peat sites, representing a range of geomorphological contexts on the South Atlantic subantarctic islands of the Falklands and South Georgia. To investigate the most suitable fraction for dating, 112 measurements were obtained from three components within selected horizons: a fine fraction 0.2 mm, and bulk material. We find site selection is critical, with locations surrounded by high-ground and/or relatively slowly accumulating sites more susceptible to the translocation of older carbon. Importantly, in locations with reduced potential for redeposition of material, our results show that there is no significant or systematic difference between ages derived from bulk material, fine or coarse (plant macrofossil) material, providing confidence in the resulting age model. Crucially, in areas comprising complex terrain with extreme relief, we recommend dating macrofossils or bulk carbon rather than a fine fraction, or employing comprehensive dating of multiple sedimentary fractions to determine the most reliable fraction(s) for developing a robust chronological framework.
    Print ISSN: 0033-8222
    Electronic ISSN: 1945-5755
    Topics: Archaeology , Energy, Environment Protection, Nuclear Power Engineering , Geosciences
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  • 9
    Publication Date: 2019-06-07
    Description: Quantitative estimates of future Antarctic climate change are derived from numerical global climate models. Evaluation of the reliability of climate model projections involves many lines of evidence on past performance combined with knowledge of the processes that need to be represented. Routine model evaluation is mainly based on the modern observational period, which started with the establishment of a network of Antarctic weather stations in 1957/58. This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends. To help address this gap, we present a new evaluation of potential ways in which long-term observational and paleo-proxy reconstructions may be used, with a particular focus on improving projections. A wide range of data sources and time periods is included, ranging from ship observations of the early 20th century to ice core records spanning hundreds to hundreds of thousands of years to sediment records dating back 34 million years. We conclude that paleo-proxy records and long-term observational datasets are an underused resource in terms of strategies for improving Antarctic climate projections for the 21st century and beyond. We identify priorities and suggest next steps to addressing this.
    Electronic ISSN: 2076-3263
    Topics: Geosciences
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  • 10
    Publication Date: 2018-11-13
    Description: The Amundsen Sea Low (ASL) plays a major role in the climate and environment of Antarctica and the Southern Ocean, including surface air temperature and sea ice concentration changes. Unfortunately, a relative dearth of observational data across the Amundsen and Bellingshausen seas prior to the satellite era (post-1979) limits our understanding of the past behaviour and impact of the ASL. The limited proxy evidence for changes in the ASL are primarily restricted to the Antarctic where ice core evidence suggests a deepening of the atmospheric pressure system during the late Holocene. However, no data have previously been reported from the northern side of the ASL. Here we report a high-resolution, multi-proxy study of a 5000-year-long peat record from the Falkland Islands, a location sensitive to contemporary ASL dynamics which modulates northerly and westerly airflow across the southwestern South Atlantic sector of the Southern Ocean. In combination with climate reanalysis, we find a marked period of wetter, colder conditions most likely the result of enhanced southerly airflow between 5000 and 2500 years ago, suggesting limited ASL influence over the region. After 2500 years ago, drier and warmer conditions were established, implying more westerly airflow and the increased projection of the ASL onto the South Atlantic. The possible role of the equatorial Pacific via atmospheric teleconnections in driving this change is discussed. Our results are in agreement with Antarctic ice core records and fjord sediments from the southern South American coast, and suggest that the Falkland Islands provide a valuable location for reconstructing high southern latitude atmospheric circulation changes on multi-decadal to millennial timescales.
    Print ISSN: 1814-9324
    Electronic ISSN: 1814-9332
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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