907 related articles for article (PubMed ID: 26840491)
1. Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age.
Jaccard SL; Galbraith ED; Martínez-García A; Anderson RF
Nature; 2016 Feb; 530(7589):207-10. PubMed ID: 26840491
[TBL] [Abstract][Full Text] [Related]
2. Evidence against dust-mediated control of glacial-interglacial changes in atmospheric CO2.
Maher BA; Dennis PF
Nature; 2001 May; 411(6834):176-80. PubMed ID: 11346790
[TBL] [Abstract][Full Text] [Related]
3. CO
Rae JWB; Burke A; Robinson LF; Adkins JF; Chen T; Cole C; Greenop R; Li T; Littley EFM; Nita DC; Stewart JA; Taylor BJ
Nature; 2018 Oct; 562(7728):569-573. PubMed ID: 30356182
[TBL] [Abstract][Full Text] [Related]
4. Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation.
Martínez-Botí MA; Marino G; Foster GL; Ziveri P; Henehan MJ; Rae JW; Mortyn PG; Vance D
Nature; 2015 Feb; 518(7538):219-22. PubMed ID: 25673416
[TBL] [Abstract][Full Text] [Related]
5. Carbon dioxide release from the North Pacific abyss during the last deglaciation.
Galbraith ED; Jaccard SL; Pedersen TF; Sigman DM; Haug GH; Cook M; Southon JR; Francois R
Nature; 2007 Oct; 449(7164):890-3. PubMed ID: 17943127
[TBL] [Abstract][Full Text] [Related]
6. Two modes of change in Southern Ocean productivity over the past million years.
Jaccard SL; Hayes CT; Martínez-García A; Hodell DA; Anderson RF; Sigman DM; Haug GH
Science; 2013 Mar; 339(6126):1419-23. PubMed ID: 23520109
[TBL] [Abstract][Full Text] [Related]
7. Centennial-scale changes in the global carbon cycle during the last deglaciation.
Marcott SA; Bauska TK; Buizert C; Steig EJ; Rosen JL; Cuffey KM; Fudge TJ; Severinghaus JP; Ahn J; Kalk ML; McConnell JR; Sowers T; Taylor KC; White JW; Brook EJ
Nature; 2014 Oct; 514(7524):616-9. PubMed ID: 25355363
[TBL] [Abstract][Full Text] [Related]
8. Iron fertilization of the Subantarctic ocean during the last ice age.
Martínez-García A; Sigman DM; Ren H; Anderson RF; Straub M; Hodell DA; Jaccard SL; Eglinton TI; Haug GH
Science; 2014 Mar; 343(6177):1347-50. PubMed ID: 24653031
[TBL] [Abstract][Full Text] [Related]
9. The Southern Ocean's role in carbon exchange during the last deglaciation.
Burke A; Robinson LF
Science; 2012 Feb; 335(6068):557-61. PubMed ID: 22174131
[TBL] [Abstract][Full Text] [Related]
10. Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes.
Gottschalk J; Skinner LC; Lippold J; Vogel H; Frank N; Jaccard SL; Waelbroeck C
Nat Commun; 2016 May; 7():11539. PubMed ID: 27187527
[TBL] [Abstract][Full Text] [Related]
11. Southern Ocean dust-climate coupling over the past four million years.
Martínez-Garcia A; Rosell-Melé A; Jaccard SL; Geibert W; Sigman DM; Haug GH
Nature; 2011 Aug; 476(7360):312-5. PubMed ID: 21814203
[TBL] [Abstract][Full Text] [Related]
12. Radiocarbon evidence for alternating northern and southern sources of ventilation of the deep Atlantic carbon pool during the last deglaciation.
Skinner LC; Waelbroeck C; Scrivner AE; Fallon SJ
Proc Natl Acad Sci U S A; 2014 Apr; 111(15):5480-4. PubMed ID: 24706801
[TBL] [Abstract][Full Text] [Related]
13. The polar ocean and glacial cycles in atmospheric CO(2) concentration.
Sigman DM; Hain MP; Haug GH
Nature; 2010 Jul; 466(7302):47-55. PubMed ID: 20596012
[TBL] [Abstract][Full Text] [Related]
14. Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release.
Rose KA; Sikes EL; Guilderson TP; Shane P; Hill TM; Zahn R; Spero HJ
Nature; 2010 Aug; 466(7310):1093-7. PubMed ID: 20740012
[TBL] [Abstract][Full Text] [Related]
15. Role of marine biology in glacial-interglacial CO2 cycles.
Kohfeld KE; Le Quéré C; Harrison SP; Anderson RF
Science; 2005 Apr; 308(5718):74-8. PubMed ID: 15802597
[TBL] [Abstract][Full Text] [Related]
16. Highly bioavailable dust-borne iron delivered to the Southern Ocean during glacial periods.
Shoenfelt EM; Winckler G; Lamy F; Anderson RF; Bostick BC
Proc Natl Acad Sci U S A; 2018 Oct; 115(44):11180-11185. PubMed ID: 30322933
[TBL] [Abstract][Full Text] [Related]
17. Carbon isotope constraints on the deglacial CO₂ rise from ice cores.
Schmitt J; Schneider R; Elsig J; Leuenberger D; Lourantou A; Chappellaz J; Köhler P; Joos F; Stocker TF; Leuenberger M; Fischer H
Science; 2012 May; 336(6082):711-4. PubMed ID: 22461496
[TBL] [Abstract][Full Text] [Related]
18. Effect of iron supply on Southern Ocean CO2 uptake and implications for glacial atmospheric CO2.
Watson AJ; Bakker DC; Ridgwell AJ; Boyd PW; Law CS
Nature; 2000 Oct; 407(6805):730-3. PubMed ID: 11048716
[TBL] [Abstract][Full Text] [Related]
19. The nature of deep overturning and reconfigurations of the silicon cycle across the last deglaciation.
Dumont M; Pichevin L; Geibert W; Crosta X; Michel E; Moreton S; Dobby K; Ganeshram R
Nat Commun; 2020 Mar; 11(1):1534. PubMed ID: 32210225
[TBL] [Abstract][Full Text] [Related]
20. Glacial greenhouse-gas fluctuations controlled by ocean circulation changes.
Schmittner A; Galbraith ED
Nature; 2008 Nov; 456(7220):373-6. PubMed ID: 19020618
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]