# | Title | Journal | Year | Citations |
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1 | A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records | Paleoceanography | 2005 | 3,308 |
2 | Glacial‐interglacial CO2 change: The Iron Hypothesis | Paleoceanography | 1990 | 1,683 |
3 | Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene | Paleoceanography | 1995 | 1,177 |
4 | Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion | Paleoceanography | 1987 | 964 |
5 | Barium in Deep‐Sea Sediment: A Geochemical Proxy for Paleoproductivity | Paleoceanography | 1992 | 963 |
6 | Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation | Paleoceanography | 1988 | 956 |
7 | Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations | Paleoceanography | 1998 | 899 |
8 | Postglacial connection of the Black Sea to the Mediterranean and its relation to the timing of sapropel formation | Paleoceanography | 1997 | 862 |
9 | Paleocean circulation during the Last Deglaciation: A bipolar seesaw? | Paleoceanography | 1998 | 846 |
10 | On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch Forcing | Paleoceanography | 1992 | 840 |
11 | On the structure and origin of major glaciation cycles 2. The 100,000‐year cycle | Paleoceanography | 1993 | 821 |
12 | Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions | Paleoceanography | 2006 | 802 |
13 | Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich events | Paleoceanography | 1993 | 745 |
14 | Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series | Paleoceanography | 2003 | 732 |
15 | Oceanic anoxic events and plankton evolution: Biotic response to tectonic forcing during the mid-Cretaceous | Paleoceanography | 2002 | 726 |
16 | Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic Ocean | Paleoceanography | 1989 | 715 |
17 | Evaluation of the Plio-Pleistocene astronomical timescale | Paleoceanography | 1996 | 685 |
18 | Midlatitude westerlies, atmospheric CO2, and climate change during the ice ages | Paleoceanography | 2006 | 676 |
19 | Evolution of Early Cenozoic marine temperatures | Paleoceanography | 1994 | 652 |
20 | A minimum thermodynamic model for the bipolar seesaw | Paleoceanography | 2003 | 628 |
21 | Astronomic timescale for the Pliocene Atlantic δ18O and dust flux records of Ocean Drilling Program Site 659 | Paleoceanography | 1994 | 614 |
22 | Changes in East Atlantic Deepwater Circulation over the last 30,000 years: Eight time slice reconstructions | Paleoceanography | 1994 | 570 |
23 | Processes controlling the organic carbon content of open ocean sediments | Paleoceanography | 1988 | 563 |
24 | Late Cenozoic Eolian deposition in the North Pacific: Asian drying, Tibetan uplift, and cooling of the northern hemisphere | Paleoceanography | 1998 | 540 |
25 | Glacial water mass geometry and the distribution of δ13C of ΣCO2in the western Atlantic Ocean | Paleoceanography | 2005 | 536 |
26 | Phase relationships between millennial-scale events 64,000-24,000 years ago | Paleoceanography | 2000 | 528 |
27 | Dansgaard-Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures | Paleoceanography | 1999 | 527 |
28 | Sortable silt and fine sediment size/composition slicing: Parameters for palaeocurrent speed and palaeoceanography | Paleoceanography | 1995 | 526 |
29 | Application of the Ce anomaly as a paleoredox indicator: The ground rules | Paleoceanography | 1990 | 520 |
30 | Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the Holocene | Paleoceanography | 1988 | 515 |
31 | Late Pliocene variation in northern hemisphere ice sheets and North Atlantic deep water circulation | Paleoceanography | 1989 | 486 |
32 | A salt oscillator in the glacial Atlantic? 1. The concept | Paleoceanography | 1990 | 472 |
33 | Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record | Paleoceanography | 2002 | 470 |
34 | Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation | Paleoceanography | 2009 | 453 |
35 | High-resolution δ13C stratigraphy through the Early Aptian “Livello selli” of the Alpine tethys | Paleoceanography | 1998 | 441 |
36 | Cadmium: Chemical tracer of deepwater paleoceanography | Paleoceanography | 1988 | 437 |
37 | Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years | Paleoceanography | 1988 | 436 |
38 | Variability of the western Mediterranean Sea surface temperature during the last 25,000 years and its connection with the Northern Hemisphere climatic changes | Paleoceanography | 2001 | 430 |
39 | Paleoenvironmental Changes in the Japan Sea During the Last 85,000 Years | Paleoceanography | 1991 | 426 |
40 | Correction of accelerator mass spectrometry 14C ages measured in planktonic foraminifera: Paleoceanographic implications | Paleoceanography | 1988 | 423 |
41 | Benthic phosphorus regeneration, net primary production, and ocean anoxia: A model of the coupled marine biogeochemical cycles of carbon and phosphorus | Paleoceanography | 1994 | 413 |
42 | Miocene evolution of atmospheric carbon dioxide | Paleoceanography | 1999 | 407 |
43 | Patterns of Ice‐Rafted Detritus in the Glacial North Atlantic (40–55°N) | Paleoceanography | 1993 | 404 |
44 | Suppression of El Niño during the Mid-Holocene by changes in the Earth's orbit | Paleoceanography | 2000 | 397 |
45 | Orbital controls on the El Niño/Southern Oscillation and the tropical climate | Paleoceanography | 1999 | 394 |
46 | The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event | Paleoceanography | 1988 | 379 |
47 | The timing of major climate terminations | Paleoceanography | 1997 | 375 |
48 | Onset of the Mid-Cretaceous greenhouse in the Barremian-Aptian: Igneous events and the biological, sedimentary, and geochemical responses | Paleoceanography | 1999 | 373 |
49 | High-resolution (104years) deep-sea foraminiferal stable isotope records of the Eocene-Oligocene climate transition | Paleoceanography | 1996 | 368 |
50 | Eastern Pacific sea surface temperature since 1600 A.D.: The δ18O record of climate variability in Galápagos Corals | Paleoceanography | 1994 | 361 |
51 | Land-ocean linkages over orbital and millennial timescales recorded in Late Quaternary sediments of the Japan Sea | Paleoceanography | 1999 | 353 |
52 | Graphic correlation of oxygen isotope stratigraphy application to the Late Quaternary | Paleoceanography | 1986 | 349 |
53 | Nannofossils and superplumes: The Early Aptian “nannoconid crisis” | Paleoceanography | 1994 | 349 |
54 | Miocene deepwater oceanography | Paleoceanography | 1989 | 346 |
55 | El Niño variability off Peru during the last 20,000 years | Paleoceanography | 2005 | 346 |
56 | The sequence of events surrounding Termination II and their implications for the cause of glacial-interglacial CO2changes | Paleoceanography | 1998 | 345 |
57 | Climatic change and CaCO3 preservation: An 800,000 year bathymetric Reconstruction from the central equatorial Pacific Ocean | Paleoceanography | 1989 | 344 |
58 | North Atlantic Deep Water cools the southern hemisphere | Paleoceanography | 1992 | 342 |
59 | Variation of atmospheric CO2by ventilation of the ocean's deepest water | Paleoceanography | 1999 | 341 |
60 | SIMMAX: A modern analog technique to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments | Paleoceanography | 1996 | 331 |
61 | Black shale deposition and faunal overturn in the Devonian Appalachian Basin: Clastic starvation, seasonal water-column mixing, and efficient biolimiting nutrient recycling | Paleoceanography | 2000 | 327 |
62 | The influence of microhabitats on the carbon isotopic composition of deep‐sea benthic foraminifera | Paleoceanography | 1990 | 326 |
63 | The Mid-Pleistocene climate transition: A deep sea carbon isotopic perspective | Paleoceanography | 1997 | 325 |
64 | A high‐resolution diatom record of the last deglaciation from the SE Norwegian Sea: Documentation of rapid climatic changes | Paleoceanography | 1992 | 321 |
65 | Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg-dependent dissolution | Paleoceanography | 1996 | 321 |
66 | Early Cenozoic decoupling of the global carbon and sulfur cycles | Paleoceanography | 2003 | 319 |
67 | The ecology of living (stained) deep-sea benthic foraminifera from the Sulu Sea | Paleoceanography | 1994 | 315 |
68 | The δ13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models | Paleoceanography | 1993 | 312 |
69 | Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas Event | Paleoceanography | 1997 | 300 |
70 | Potential links between surging ice sheets, circulation changes, and the Dansgaard-Oeschger Cycles in the Irminger Sea, 60-18 Kyr | Paleoceanography | 2000 | 299 |
71 | A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution | Paleoceanography | 1995 | 293 |
72 | Onset of “Hudson Strait” Heinrich events in the eastern North Atlantic at the end of the middle Pleistocene transition (∼640 ka)? | Paleoceanography | 2008 | 290 |
73 | Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: Reinterpreting cave speleothemδ18O | Paleoceanography | 2010 | 289 |
74 | Glacial North Atlantic: Sea-surface conditions reconstructed by GLAMAP 2000 | Paleoceanography | 2003 | 288 |
75 | Oxygen Isotopic Composition of Multiple Species of Planktonic Foraminifera: Recorders of the Modern Photic Zone Temperature Gradient | Paleoceanography | 1992 | 285 |
76 | Fluctuations in the trophic resource continuum: A factor in global diversity cycles? | Paleoceanography | 1987 | 283 |
77 | Benthic foraminiferal δ13C and accumulation rates of organic carbon: Uvigerina Peregrina group and Cibicidoides Wuellerstorfi | Paleoceanography | 1986 | 280 |
78 | Origin of the Middle Pleistocene Transition by ice sheet erosion of regolith | Paleoceanography | 1998 | 280 |
79 | 230Th normalization: An essential tool for interpreting sedimentary fluxes during the late Quaternary | Paleoceanography | 2004 | 278 |
80 | Slow dynamics of the Northern Hemisphere glaciation | Paleoceanography | 2005 | 272 |
81 | Variations in Atlantic surface ocean paleoceanography, 50°-80°N: A time-slice record of the last 30,000 years | Paleoceanography | 1995 | 271 |
82 | Glacial-age hydrography of the far northwest Pacific Ocean | Paleoceanography | 1998 | 271 |
83 | Early and Middle Miocene stable isotopes: Implications for Deepwater circulation and climate | Paleoceanography | 1992 | 270 |
84 | Strontium/calcium ratios in modernporitescorals From the Great Barrier Reef as a proxy for sea surface temperature: Calibration of the thermometer and monitoring of ENSO | Paleoceanography | 1997 | 270 |
85 | The 41 kyr world: Milankovitch's other unsolved mystery | Paleoceanography | 2003 | 267 |
86 | Enhanced productivity led to increased organic carbon burial in the euxinic North Atlantic basin during the late Cenomanian oceanic anoxic event | Paleoceanography | 2002 | 266 |
87 | Orbital climate forcing of δ13C excursions in the late Paleocene-early Eocene (chrons C24n-C25n) | Paleoceanography | 2003 | 266 |
88 | Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years | Paleoceanography | 1998 | 265 |
89 | Late Pleistocene variability of Arabian Sea summer monsoon winds and continental aridity: Eolian records from the lithogenic component of deep‐sea sediments | Paleoceanography | 1990 | 263 |
90 | Dust impact on marine biota and atmospheric CO2during glacial periods | Paleoceanography | 2003 | 263 |
91 | Carbon isotope ratio of Cenozoic CO2: A comparative evaluation of available geochemical proxies | Paleoceanography | 2010 | 262 |
92 | Sensitivity of the Atlantic Intertropical Convergence Zone to Last Glacial Maximum boundary conditions | Paleoceanography | 2003 | 261 |
93 | Thermal evolution of Cretaceous Tethyan marine waters inferred from oxygen isotope composition of fish tooth enamels | Paleoceanography | 2003 | 260 |
94 | Basinal restriction, black shales, Re‐Os dating, and the Early Toarcian (Jurassic) oceanic anoxic event | Paleoceanography | 2008 | 257 |
95 | Coupled greenhouse warming and deep‐sea acidification in the middle Eocene | Paleoceanography | 2009 | 251 |
96 | Carbonate Dissolution Fluctuations in the Western Equatorial Pacific During the Late Quaternary | Paleoceanography | 1992 | 249 |
97 | Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian‐Turonian Oceanic Anoxic Event | Paleoceanography | 2011 | 248 |
98 | Rapid analysis of high-precision Sr/Ca ratios in corals and other marine carbonates | Paleoceanography | 1999 | 244 |
99 | Stochastic resonance in the North Atlantic | Paleoceanography | 2001 | 244 |
100 | A resolution for the coiling direction paradox inNeogloboquadrina pachyderma | Paleoceanography | 2006 | 243 |