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 | Journal of Paleolimnology 2002, Vol 28 |
A Luzon, A Gonzalez, A Munoz, B SanchezValverde | Upper Oligocene-Lower Miocene shallowing-upward lacustrine sequences controlled by periodic and non-periodic processes (Ebro Basin, northeastern Spain) | 441-456 |
B Beierle, J Bond | Density-induced settling of tephra through organic lake sediments | 433-440 |
DF Porinchu, GM MacDonald, AM Bloom, KA Moser | The modern distribution of chironomid sub-fossils (Insecta : Diptera) in the Sierra Nevada, California: Potential for paleoclimatic reconstructions | 355-375 |
E Gandouin, E Franquet | Late Glacial and Holocene chironomid assemblages in 'Lac Long Inferieur' (Southern France, 2090 m): palaeoenvironmental and palaeoclimatic implications | 317-328 |
EL Bredesen, DG Bos, KR Laird, BF Cumming | A cladoceran-based paleolimnological assessment of the impact of forest harvesting on four lakes from the central interior of British Columbia, Canada | 389-402 |
F GarciaRodriguez, N Mazzeo, P Sprechmann, D Metzeltin, F Sosa, HC Treutler, M Renom, B Scharf, C Gaucher | Paleolimnological assessment of human impacts in Lake Blanca, SE Uruguay | 457-468 |
IS Spooned, D Mazzucchi, G Osborn, R Gilbert, I Larocques | A multi-proxy holocene record of environmental change from the sediments of Skinny Lake, Iskut region, northern British Columbia, Canada | 419-431 |
JQ Yu, KR Kelts | Abrupt changes in climatic conditions across the late-glacial/Holocene transition on the N. E. Tibet-Qinghai Plateau: evidence from Lake Qinghai, China | 195-206 |
K SarmajaKorjonen | Multi-proxy data from Kaksoislammi Lake in Finland: dramatic changes in the late Holocene cladoceran assemblages | 287-296 |
KA Moser, JP Smol, GM MacDonald, CPS Larsen | 19th century eutrophication of a remote boreal lake: a consequence of climate warming? | 269-281 |
KW Keatings, THE Heaton, JA Holmes | The effects of diagenesis on the trace element and stable isotope geochemistry of non-marine ostracod valves | 245-252 |
MFJ Pisaric | Long-distance transport of terrestrial plant material by convection resulting from forest fires | 349-354 |
N Michelutti, MSV Douglas, JP Smol | Tracking recent recovery from eutrophication in a high arctic lake (Meretta Lake, Cornwallis Island, Nunavut, Canada) using fossil diatom assemblages | 377-381 |
P Francus, F Keimig, M Besonen | An algorithm to aid varve counting and measurement from thin-sections | 283-286 |
PA Meyers | Evidence of mid-Holocene climate instability from variations in carbon burial in Seneca Lake, New York | 237-244 |
R Nunez, B Spiro, A Pentecost, A Kim, P Coletta | Organo-geochemical and stable isotope indicators of environmental change in a marl lake, Malham Tarn, North Yorkshire, UK | 403-417 |
RK Booth | Testate amoebae as paleoindicators of surface-moisture changes on Michigan peatlands: modern ecology and hydrological calibration | 329-348 |
RT Patterson, A Dalby, A Kumar, LA Henderson, REA Boudreau | Arcellaceans (Thecamoebians) as indicators of land-use change: settlement history of the Swan Lake area, Ontario as a case study | 297-316 |
S Brown, P Bierman, A Lini, PT Davis, J Southon | Reconstructing lake and drainage basin history using terrestrial sediment layers: analysis of cores from a post-glacial lake in New England, USA | 219-236 |
S Palmer, I Walker, M Heinrichs, R Hebda, G Scudder | Postglacial midge community change and Holocene palaeotemperature reconstructions near treeline, southern British Columbia (Canada) | 469-490 |
SR Verkulich, M Melles, HW Hubberten, ZV Pushina | Holocene environmental changes and development of Figurnoye Lake in the southern Bunger Hills, East antarctica | 253-267 |
U Kienel, T Kumke | Combining ordination techniques and geostatistics to determine the patterns of diatom distributions at Lake Lama, Central Siberia | 181-194 |
ZC Yu, E Ito, DR Engstrom | Water isotopic and hydrochemical evolution of a lake chain in the northern Great Plains and its paleoclimatic implications | 207-217 |