Environmental processes of the ice age: Land, oceans, glaciers (EPILOG)

Quaternary Science Reviews

Volumn 20, Issue 4, 2001, Pages 627-657

  Mix, Alan C ^a   Bard, Edouard ^b   Schneider, Ralph ^c  

^a OREGON STATE UNIVERSITY   (United States)

^b CEREGE   (France)

^c UNIVERSITY OF BREMEN   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ENVIRONMENTAL CHANGE; LAND SURFACE; LAST GLACIAL MAXIMUM; OCEANOGRAPHY;

DELMENHORST; GERMANY;

EID: 0035113983     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0277-3791(00)00145-1     Document Type: Article

References (251)

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2. Spatial distribution pattern of living polycistine radiolarian taxa: Baseline study for paleoenvironmental reconstructions in the Southern Ocean (Atlantic Sector)
3. Strontium/calcium ratios in modern Porites corals from the Great Barrier Reef as a proxy for sea surface temperature: Calibration of the thermometer and monitoring of ENSO
4. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event
5. Visual-stratigraphic dating of the GISP2 ice core: Basis, reproducibility, and application
6. Geochemical anomalies in coral skeletons and their possible implications for palaeoenvironmental analyses
7. Incorporation of uranium in modern corals
8. Estimates of sea-surface temperature in the Coral Sea at the Last Glacial Maximum
9. Tropical Pacific Ocean thermocline depth reconstructions for the Last Glacial Maximum
10. An ocean of ice - Advances in the estimation of past sea ice in the Southern Ocean
11. Ice age temperatures and geochemistry
12. 18O spectra from deep-sea cores
13. 14C ages of corals. An updated database including samples from Barbados, Mururoa and Tahiti
14. 14C gradient during the Younger Dryas climate event
15. Deglacial sea level record from Tahiti corals and the timing of global meltwater discharge
16. 14C timescale over the past 130,000 years using mass spectrometric U-Th ages from Barbados corals
17. U/Th ages obtained by mass spectrometry in corals from Barbados: Sea level during the past 130,000 years
18. Inter-hemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry
19. Hydrological impact of Heinrich events in the subtropical northeast Atlantic
20. On the inclusion of trace materials into massive coral skeleton. Part II: Distortions in skeletal records of annual climate cycles due to growth processes
21. Sea-surface temperatures of the southwest Pacific Ocean during the Last Glacial Maximum
22. Subtropical convergence fluctuations and Quaternary climates in the middle latitudes of the Indian Ocean
23. Primary production response to orbitally induced variations of the southern oscillation in the equatorial Indian Ocean
24. Abrupt changes in early Holocene tropical sea surface temperatures derived from coral records
25. High precision correlations of Greenland and Antarctic ice core records over the last 100 kyr
26. Anomalously low alkenone temperatures caused by lateral particle and sediment transport in the Malvinas Current region, western Argentine Basin
27. On the determination of Pleistocene temperatures from planktonic foraminifera
28. Tropical boundary layer equilibrium in the last ice age
29. Asynchrony of Antarctic and Greenland climate change during the last glacial period
30. 2 increase with respect to the Younger Dryas event
31. 18O measured from Acropora nobilis and Porites lutea: Is Sr/Ca paleothermometry always reliable?
32. Evidence for massive discharges of icebergs into the North Atlantic Ocean during the last glacial period
33. Paleoclimatic signals recognized by chemometric treatment of molecular stratigraphic data
34. Late Quaternary variations in sea surface temperatures and their relationship to orbital forcing recorded in the Southern Ocean (Atlantic sector)
35. Tropical cooling at the Last Glacial Maximum: An atmosphere-mixed layer ocean model simulation
36. Comparing simulated glacial climate and paleodata: A reexamination
37. Oxygen isotope constraints on surface ocean temperatures
38. 16O record for the last deglaciation
39. Preliminary estimates for the radiocarbon age of deep water in the glacial ocean
40. Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by depositional dissolution: Evidence of shallow Mg-dependent dissolution
41. Diatom distribution and paleoceanographic reconstruction in the Southern Ocean: Present and Last Glacial Maximum
42. Sea-ice extent in the Southern Ocean during the Last Glacial Maximum: Another approach to the problem
43. Reappraisal of sea-ice distribution in the Atlantic and Pacific sectors of the Southern Ocean at 18,000 yr BP
44. The role of ocean-atmosphere interactions in tropical cooling during the last glacial maximum
45. 18O records in massive corals from Bermuda: Relationships with sea-surface temperatures
46. The last deglaciation in the Eastern Arabian Sea: Planktonic foraminiferal and alkenone records
47. Paleoproductivity in the equatorial Indian Ocean for the last 260,000 yr: A transfer function based on planktonic foraminifera
48. Faunal and alkenone reconstructions of subtropical North Atlantic surface hydrography and paleotemperature over the last 28 kyr
49. Climate connections between the hemispheres revealed by deep-sea sediment core/ice core correlations
50. Origin of the first global meltwater pulse following the last glacial maximum
51. Northern hemisphere ice-sheet influences on global climate change
52. Ice sheets by volume
53. The surface of the ice-age earth
54. Seasonal reconstruction of the earth's surface at the last glacial maximum
55. Climatic changes of the last 18,000 years: Observations and model simulations
56. Amazonian and neotropical plant communities on glacial time-scales: The failure of the aridity and refuge hypotheses
57. Genetic and physiological influences on the alkenone/alkenoate versus growth temperature relationship in Emiliania huxleyi and Gephyrocapsa oceanica
58. Estimates of Antarctic Ocean seasonal sea-ice cover during glacial intervals
59. Changes in sea surface hydrology associated with Heinrich event 4 in the North Atlantic Ocean between 40° and 60°N
60. U, Sr and Mg in Holocene and Pleistocene corals
61. Application of modern analog technique to marine Antarctic diatoms: Reconstruction of maximum sea ice extent at the Last Glacial Maximum
62. Reappraisal of Antarctic seasonal sea ice at the last glacial maximum
63. CLIMAP SSTs re-revisited
64. Effect of vegetation on an ice-age climate model simulation
65. Large Arctic temperature change at the Wisconsin-Holocene glacial transition
66. Evidence for general instability of past climate from a 250-kyr ice-core record
67. Oxygen 18-salinity relationship simulated by an oceanic general circulation model
68. Sea-ice cover, sea-surface salinity, and halo-/thermocline structure of the northwest North Atlantic: Modern versus full glacial conditions
69. Micropaleontology and palynology of core PAR87A-10: A 23,000-year record of paleoenvironmental changes in the Gulf of Alaska, northeast North Pacific
70. Dinoflagellate cyst distribution in high-latitude marine environments and quantitative reconstruction of sea-surface salinity, temperature, and seasonality
71. Seawater strontium and Sr/Ca variability in the Atlantic and Pacific oceans
72. 18O reconstructions of sea surface temperatures
73. The Sr/Ca-temperature relationship in coralline aragonite: Influence of variability in (Sr/Ca) seawater and skeletal growth parameters
74. Isotopic composition of photosynthetic oxygen
75. Biomarker temperature estimates for modern and last glacial surface waters of the California Current system between 33° and 42°N
76. How fast did the ocean-atmosphere system run during the last deglaciation?
77. North Atlantic deepwater temperature change during Late Pliocene and Late Quaternary climatic cycles
78. 230Th ages of corals
79. 18O of surface seawaters inferred from foraminiferal Mg/Ca ratios
80. Millennial-scale iceberg discharges in the Irminger Basin during the last glacial period: Relationship with the Heinrich events and environmental settings
81. Pleistocene temperatures
82. An effect of dissolved nutrient concentration on alkenone based temperature estimates
83. A 17,000-year glacio-eustatic sea level record: Influence of glacial melting rates on the Younger Dryas event and deep ocean circulation
84. Tropical climates at the Last Glacial Maximum: A new synthesis of terrestrial palaeoclimate data. I. Vegetation, lake-levels, and geochemistry
85. 2 around the last three glacial terminations
86. Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites
87. Simulation of modern and glacial climates with a coupled global model of intermediate complexity
88. Modeling the ice-age climate
89. Modern Pacific coccolith assemblages: Derivation and application to late Pleistocene paleotemperature analysis
90. Strontianite in coral skeletal aragonite
91. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores
92. Tropical temperature variations since 20,000 years ago: Modulating interhemispheric climate change
93. Electrical conductivity method (ECM) and stratigraphic dating of the Byrd station ice core Antarctica
94. Rapid flooding of the Sunda Shelf: A late-glacial sea-level record
95. An ion probe study of annual cycles of Sr/Ca and other trace elements in corals
96. Foraminiferal magnesium in Globigerinoides sacculifer as a paleotemperature proxy
97. Reconstruction of the Atlantic and western Indian Ocean sectors of the 18,000 BP Antarctic Ocean
98. Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years
99. Latest Quaternary North Pacific surface-water responses imply atmosphere-driven climate instability
100. Depth and seasonality of alkenone production along the California margin inferred from a core top transect
101. Glacial-interglacial sea-surface temperature record inferred from alkenone indices, Site 893, Santa Barbara Basin
102. Reassessment of ice-age cooling of the tropical ocean and atmosphere
103. The last great ice sheets: A global view
104. Transfer functions under no-analog conditions: Experiments with Indian Ocean planktonic foraminifera
105. The Agulhas Current during the late Pleistocene: Analysis of modern faunal analogs
106. A new micropaleontological method for quantitative paleoclimatology: Application to a late Pleistocene Caribbean core
107. Oceanic response to orbital forcing in the late Quaternary: Observational and experimental strategies
108. On the structure and origin of major glaciation cycles 2. The 100,000-year cycle
109. 2+) into the skeleton of the hermatypic coral Galaxea fascicularis
110. Are calcium and strontium transported by the same mechanism in the hermatypic coral Galaxea fascicularis?
111. 18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability
112. Greenland paleotemperatures derived from GRIP bore hole temperature and ice core isotope profiles
113. Oxygen isotope profiles through the Antarctic and Greenland ice sheets
114. Glacial-age hydrography of the far northwest Pacific Ocean
115. Laurentide ice sheet meltwater recorded in Gulf of Mexico deep-sea cores
116. New transfer function for estimating past sea surface conditions from seabed distribution of planktonic forminiferal assemblages in the North Atlantic
117. 14C calibration curve
118. Neogloboquadrina pachyderma (sinistral coiling) as paleoceanographic tracers in polar oceans: Evidence from Northeast Water Polynya plankton tows, sediment traps, and surface sediments
119. The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18,000 years
120. Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years
121. Global ice volumes at the Last Glacial Maximum and early Lateglacial, 2000
122. Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing
123. Climate impact of late Quaternary equatorial Pacific sea-surface temperature variations
124. Cool surface waters of the subtropical North Pacific Ocean during the last glacial
125. Relationship of radiolarian assemblages to sediment types and physical oceanography in the Atlantic and western Indian Ocean sectors of the Antarctic Ocean
126. Millennial-scale deep water oscillations: Reflections of the North Atlantic in the deep Pacific from 10 to 60 ka
127. Early diagenesis of lipid biomarker compounds in North Atlantic sediments
128. Application of artificial neural networks to paleoceanographic data
129. Simulation of the tropical climate of an ice age
130. Long chain (n-C37-C39) alkenones in the Prymnesiophyceae: Distributions of alkenones and other lipids and their taxonomic significance
131. Variation of foraminiferal Sr/Ca over Quaternary glacial-interglacial cycles: Evidence for changes in mean ocean Sr/Ca?
132. 18O -water using foraminiferal Mg
133. Coccoliths as paleoclimatic indicators of Pleistocene glaciations
134. Glacial North Atlantic years ago: A CLIMAP reconstruction
135. The Greenland Ice Sheet Project 2 depth-age scale: Methods and results
136. Preliminary depth-age scale of the GISP2 ice core
137. Glacial-Holocene carbonate dissolution and sea surface temperatures in the South China and Sulu Seas
138. Annual cycles of U/Ca in coral skeletons and U/Ca thermometry
139. The oxygen-isotope record of glaciation
140. Pleistocene paleoproductivity: Evidence from organic carbon and foraminiferal species
141. The marine oxygen-isotope record: Constraints on timing and extent of ice growth events (120-65 ka)
142. Climate feedback and Pleistocene variations in the Atlantic South Equatorial Currents
143. Oxygen isotope analyses and deep-sea temperature changes: Implications for rates of oceanic mixing
144. Oxygen-isotope analyses and Pleistocene ice volumes
145. Structure and timing of the last deglaciation: Oxygen-isotope evidence
146. Late Quaternary paleoceanography of the tropical Atlantic, 1, spatial variability of annual mean sea surface temperatures, 0-20,000 years B.P.
147. Late Quaternary paleoceanography of the tropical Atlantic, II: The seasonal cycle of sea-surface temperatures, 0-20,000 years B.P.
148. Foraminiferal faunal estimates of paleotemperatures: Circumventing the no-analog problem yields cool ice-age tropics
149. Rapid climate oscillations in the Northeast Pacific during the last deglaciation reflect northern and southern hemisphere sources
150. Comparison of foraminiferal, coccolithophorid, and radiolarian paleotemperature equations: Assemblage coherency and estimate concordancy
151. The reconstruction of sea surface temperatures in the Pacific Ocean of 18,000 B.P.
152. The biological record of the ice age ocean
153. Planktonic foraminifera as recorders of past surface-water stratification
154. k′ based on core-tops from the eastern South Atlantic and global ocean (60°N-60°S)
155. The transition from the last glacial period in inland and near-coastal Antarctica
156. Assessing the reliability of magnesium in foraminiferal calcite as a proxy for water mass temperature
157. k′, oxygen isotopes, and foraminiferal transfer function
158. Small changes in the sea surface temperature during the last 20,000 years: Molecular evidence from the western tropical Pacific
159. Depth ranges of alkenone production in the central Pacific Ocean
160. Comparison of Imbrie-Kipp transfer function and modern analog temperature estimates using sediment trap and core top foraminiferal faunas
161. The California Current of the last glacial maximum: Reconstruction at 42°N based on multiple proxies
162. Faunal and solution patterns of planktonic foraminifera in surface sediments of the South Pacific
163. Late Quaternary climatic changes in western tropical Africa deduced from deep-sea sedimentation off the Niger delta
164. Ice age paleotopography
165. "Implicit ice" in the global theory of glacial isostatic adjustment
166. Postglacial variations in the level of the sea: Implications for climate dynamics and solid-earth geophysics
167. 2
168. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica
169. Sensitivity of northern hemisphere air temperatures and snow expansion to North Pacific sea surface temperatures in the Goddard Institute for Space Studies general circulation model
170. The continental record of environmental conditions at 18,00 yr B.P.: An initial evaluation
171. SIMMAX: A modern analog technique to deduce Atlantic sea surface temperatures from planktonic foraminifera in deep-sea sediments
172. Surface water temperature changes in the high latitudes of the southern hemisphere during the last glacial-interglacial cycle
173. k′ and diatom assemblage sea surface temperature estimates with atlas derived data in Holocene sediments from the Southern West Indian Ocean
174. Tropical paleoclimates at the Last Glacial Maximum: Comparison of Paleoclimate Modeling Intercomparision Project (PMIP) simulations and paleodata
175. Spatial and temporal oceanographic variability of the eastern equatorial Pacific during the late Pleistocene: Evidence from Radiolaria microfossils
176. Radiolarian-based transfer functions for estimating mean surface ocean temperatures and seasonal range
177. Does growth rate affect ketone unsaturation and intracellular carbon isotopic variability in Emiliania huxleyi?
178. A biomarker perspective on prymnesiophyte productivity in the northeast Pacific Ocean
179. Post-depositional stability of long-chain alkenones under contrasting redox conditions
180. Assessment of sea-surface temperature at 42°N in the California Current over the last 30,000 years
181. Calibration of unsaturation patterns in long-chain ketone compositions for paleotemperature assessment
182. The stability of low-latitude sea-surface temperatures: An evaluation of the CLIMAP reconstruction with emphasis on the positive SST anomalies
183. Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle
184. Sensitivity experiments to sea surface temperatures, sea-ice extent, and ice-sheet reconstructions for the last glacial maximum
185. Using planktonic foraminifera as monitors of the tropical surface ocean
186. Reconstructing tropical Atlantic hydrography using planktonic foraminifera and an ocean model
187. Terrestrial conditions at the Last Glacial Maximum and CLIMAP sea-surface temperature estimates: Are they consistent?
188. 18O: A critical assessment
189. Interhemispheric appraisal of the value of alkenone indices as temperature and salinity proxies in high-latitude locations
190. Project takes a new look at past sea surface temperatures
191. k′ to estimate low sea surface temperature?
192. Factors controlling the fluoride content of planktic foraminifera
193. 16O of seawater
194. Sea surface temperature changes in the Northeastern Pacific ocean during the past 20,000 years and their relationship to climate change in Northwestern North America
195. Variations in Atlantic surface ocean paleoceanography 50°-80°N: A time-slice record of the last 30,000 years
196. Error analysis of paleosalinity calculations
197. Late Quaternary surface temperatures and productivity in the east-equatorial South Atlantic; response to changes in trade/monsoon wind forcing and surface water advection
198. Atlantic alkenone sea-surface temperature records: Low versus mid latitudes and differences between hemispheres
199. Rapid determination of high-precision Sr/Ca ratios in corals and other marine carbonates
200. 18O of seawater in the deep ocean during the Last Glacial Maximum
201. Pore fluid constraints on the temperature and oxygen isotopic composition of the glacial ocean
202. Oxygen isotopic analyses and Pleistocene temperatures re-assessed
203. The oxygen isotope stratigraphic record of the late Pleistocene
204. Oxygen isotopes, ice volume and sea level
205. Radiocarbon age of last glacial Pacific deep water
206. Environmental controls on uranium in reef corals
207. The calibration of D(Sr/Ca) versus sea surface temperature relationship fot Porites corals
208. 18O and foraminiferal assemblage temperature estimates
209. A reexamination of northeast Atlantic sea surface temperature and salinity over the last 16 kyr
210. Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation
211. Calibration of long-chain alkenone unsaturation ratios for palaeotemperature estimation in cold polar waters
212. Alkenones and alkenes in surface waters and sediments of the Southern Ocean: Implications for paleotemperature estimation in polar regions
213. High resolution analysis of trace elements in corals by laser ablation ICP-MS
214. Temperature and salinity effects on alkenones ratios measured in surface sediments from the Indian Ocean
215. Climate records covering the last deglaciation
216. Synchronous climate changes in Antarctica and the North Atlantic
217. 2 variations
218. Effects of Quaternary sea level cycles on strontium in seawater
219. GISP2 oxygen isotope ratios
220. INTCAL98 radiocarbon age calibration, 24,000-0 cal BP
221. Cooling of tropical Brazil (5°C) during the Last Glacial Maximum
222. The strontium, magnesium and sodium composition of recent scleractinian coral skeletons as standards for palaeoenvironmental analysis
223. Microbial degradation of the prymnesiophyte Emiliania huxleyi under oxic and anoxic conditions as a model for early diagenesis: Long chain alkadienes, alkenones and alkyl alkenoates
224. Late glacial stage and Holocene tropical ice core records from Huascarán, Peru
225. Rock magnetic detection of distal ice-rafted debries: Clue for the identification of Heinrich layers on the Portuguese margin
226. Sea-surface temperature estimates for the tropical western Pacific during the last glaciation and their implications for the Pacific warm pool
227. Some further inputs
228. Improving past sea surface temperature estimates based on planktonic fossil faunas
229. Testing the effects of tropical temperature, productivity, and mixed-layer depth on foraminiferal transfer functions
230. Simulated influence of carbon dioxide, orbital forcing, and ice sheets on the climate of the Last Glacial Maximum
231. Combined coccolith, foraminiferal, and biomarker reconstruction of paleoceanographic conditions over the past 120 kyr in the northern North Atlantic (59°N, 23°W)
232. Influence of ocean heat transport on the climate of the Last Glacial Maximum
233. Incorporation of strontium into reef coral skeletal carbonate
234. Late Quaternary surface circulation of the South Atlantic: The stable isotope record and implications for heat transport and productivity
235. Ice-free Nordic seas during the Last Glacial Maximum?. Potential sites of deepwater formation
236. How do radiolarian sediment assemblages reflect the ecology of the surface ocean?
237. Response of the tropical Atlantic thermocline to late Quaternary trade wind changes
238. The importance of tropical sea surface temperature patterns in sumulations of Last Glacial Maximum climate
239. Timing for the maximum of the Last Glacial constrained by lowest sea-level observations
240. Behaviour of magnesium and strontium during the transformation of coral aragonite to calcite in aquatic environments
241. 18O in the oceans temperature-salinity-density field: Constraints on ice-age thermohaline circulation
242. Water mass conversion in the glacial subarctic Pacific (54°N, 148°W). Physical constraints and the benthic-planktonic stable isotope record
243. Atmospheric freshwater fluxes and their effect on the global thermohaline circulation
244. Diatom distributions in southern ocean surface sediments (Atlantic sector): Implications for paleoenvironmental reconstructions