The Stratigraphic Record of Deep-Sea Cores and Its Implications for the Assessment of Glacials, Interglacials, Stadials, and Interstadials in the Mid-PleistoceneSHACKLETON N. J.World Anthropology. 1975, Vol p. vol, pp 1-24Article

STABLE ISOTOPE STUDY OF THE PALAEOENVIRONMENT OF THE NEOLITHIC SITE OF NEA NIKOMEDEIA, GREECE.SHACKLETON N.1970; NATURE-G.B.; 1970(8), VOL. 227, NUM. 5261, P. 943 A 944Miscellaneous

DEPTH OF PELAGIC FORAMINIFERA AND ISOTOPIC CHANGES IN PLEISTOCENE OCEANS.SHACKLETON N.1968; NATURE.; 1968(4), VOL. 218, NUM. 5136, P. 79 A 80Miscellaneous

OXYGEN AND CARBON ISOTOPE RECORD THROUGH THE OLIGOCENE, DSDP SITE 366, EQUATORIAL ATLANTIC.BOERSMA A; SHACKLETON N.1978; IN: INITIAL REP. DEEP SEA DRILLING PROJ. ABIDJAN, IVORY COAST TO MALAGA, SPAIN; 1975; WASHINGTON; U.S. GOV. PRINT. OFF.; DA. 1978; VOL. 41; PP. 957-962; BIBL. 18 REF.; 4 ILL.; 15 ANAL.Book Chapter

THE CLIMATE OF THE EOCENE OCEAN = LE CLIMAT DE L'OCEAN A L'EOCENESHACKLETON N; BOERSMA A.1981; J. GEOL. SOC. (LOND.); ISSN 0016-7649; GBR; DA. 1981; VOL. 138; NO 2; PP. 153-157; BIBL. 24 REF.Article

PARALLEL CHANGES IN SPECIES DIVERSITY AND PALAEOTEMPERATURE IN THE LOWER MIOCENEJENKINS DG; SHACKLETON N.1979; NATURE; GBR; DA. 1979; VOL. 5699; NO 278; PP. 50-51; BIBL. 12 REF.Article

Deep trouble for climate change = Etude des variations climatiquesSHACKLETON, N. J.Nature (London). 1989, Vol 342, Num 6250, pp 616-617, issn 0028-0836Article

Paleogene stable isotope events = Evénements paléogènes à partir d'isotopes stablesSHACKLETON, N. J.Palaeogeography, palaeoclimatology, palaeoecology. 1986, Vol 57, Num 1, pp 91-102, issn 0031-0182, no spécialArticle

Boundaries and events in the Paleogene = Limites et événements au PaléogèneSHACKLETON, N. J.Palaeogeography, palaeoclimatology, palaeoecology. 1986, Vol 57, Num 1, issn 0031-0182, 117 p., no spécialSerial Issue

Oxygen isotope evidence for Cenozoic climatic change = Mise en évidence au moyen des isotopes d'oxygène du changement climatique au CénozoïqueSHACKLETON, N. J.Geological journal. Special issue. 1984, Num 11, pp 27-34, issn 0435-3951Article

LATE NEOGENE PLANKTONIC FORAMINIFERA AND OXYGEN ISOTOPES: PALEOOCEANOGRAPHY IN SOUTH PACIFIC DSDP SITES.KENNETT J; MALMGREN B; SHACKLETON N et al.1977; GEOL. SOC. AMER., ABSTR. PROGRAMS; U.S.A.; DA. 1977; VOL. 9; NO 7; PP. 1047-1048Conference Paper

The δ¹⁸O spectrum of oceanic deep water over a five―decade band = Etude du spectre isotopique O¹⁸/O¹⁶ des eaux profondes océaniques sur une bande de cinq décades de fréquenceSHACKLETON, N. J; IMBRIE, J.Climatic change. 1990, Vol 16, Num 2, pp 217-230, issn 0165-0009Article

RECONSTRUCTION OF THE ATLANTIC AND WESTERN INDIAN OCEAN SECTORS OF THE 18,000 B.P. ANTARCTIC OCEAN.HAYS JD; LOZANO JA; SHACKLETON N et al.1976; GEOL. SOC. AMER., MEM.; U.S.A.; DA. 1976; NO 145; PP. 337-372; BIBL. 2 P. 1/2; 20 ILL.Article

Are teachers' judgements of pupils' ability influenced by body shape?SHACKLETON, N. L; CAMPBELL, T.International journal of obesity. 2014, Vol 38, Num 4, pp 520-524, issn 0307-0565, 5 p.Article

Oxygen isotopes and sea level = Isotopes de l'oxygène et niveau de la merCHAPPELL, J; SHACKLETON, N. J.Nature (London). 1986, Vol 324, Num 6093, pp 137-140, issn 0028-0836Article

RADIOLARIAN ESTIMATED SEA SURFACE TEMPERATURE MAP OF THE ATLANTIC AN WESTERN INDIAN SECTORS OF THE ANTARCTIC OCEAN AT 17,000 YEARS B.P.LOZANO J; HAYS JD; SHACKLETON N et al.1973; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; DA. 1973; VOL. 5; NO 7; PP. 720Article

Two proximal, high-resolution records of foraminiferal fragmentation and their implications for changes in dissolutionPFUHL, H. A; SHACKLETON, N. J.Deep-sea research. Part 1. Oceanographic research papers. 2004, Vol 51, Num 6, pp 809-832, issn 0967-0637, 24 p.Article

The use of amine complexes in managing inadvertent activation of pyroxene in a pentlandite-pyroxene flotation systemSHACKLETON, N. J; MALYSIAK, V; O'CONNOR, C. T et al.Minerals engineering. 2003, Vol 16, Num 9, pp 849-856, issn 0892-6875, 8 p.Article

Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene = Preuve de cyclicités de 550 et 1000 ans dans les modèles de circulation de Atlantique nord pendant l'HolocèneCHAPMAN, M. R; SHACKLETON, N. J.The Holocene (Sevenoaks). 2000, Vol 10, Num 3, pp 287-291, issn 0959-6836Article

The evolution of oceanic oxygen-isotope variability in the North Atlantic over the past three million years. Discussion = Evolution de la variabilité isotopique de l'oxygène océanique dans l'Atlantique Nord au cours des trois derniers millions d'années. DiscussionSHACKLETON, N. J; IMBRIE, J; PISLAS, N. G et al.Philosophical transactions of the Royal Society of London. Series B, Biological sciences. 1988, Vol 318, Num 1191, pp 679-688, issn 0080-4622Conference Paper

Modelling the global climate response to orbital forcing and atmospheric carbon dioxide changes = Modélisation de la réponse climatique mondiale au forçage orbital et aux variations atmosphériques du dioxyde de carbonePISIAS, N. G; SHACKLETON, N. J.Nature (London). 1984, Vol 310, Num 5980, pp 757-759, issn 0028-0836Article

The effect of accumulation rate on the spectrum of geologic time series: evidence from two South Atlantic sediment cores = L'effet du taux d'accumulation sur le spectre des séries de temps géologique: évidence à partir de deux carottes de sédiments de l'Atlantique SudMORLEY, J. J; SHACKLETON, N. J.Milankovitch and climate; understanding the response to astronomical forcing: NATO advanced research. Workshop. 1984, pp 467-480Conference Paper

How accurate are our chronologies of the past ?BARD, E; STUIVER, M; SHACKLETON, N et al.Dahlem workshop on global changes in the perspective of the past. 1993, pp 103-120Conference Paper

An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677SHACKLETON, N. J; BERGER, A; PELTIER, W. R et al.Transactions of the Royal Society of Edinburgh. Earth sciences. 1990, Vol 81, Num 4, pp 251-261, issn 0263-5933Conference Paper

Response of global deep-water circulation to Earth's climatic change 135,000-107,000 years ago = Réponse de la circulation des eaux profondes dans le Monde aux variations climatiques de la Terre il y a 135000 ans et 107000 ansDUPLESSY, J.-C; SHACKLETON, N. J.Nature (London). 1985, Vol 316, Num 6028, pp 500-507, issn 0028-0836Article