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All ICDP Publications with Abstracts

From parent-sysfolder "Publications" + 2 folder-levels deep

128.
Koval, P.V.; Gvozdkov, A.N.; Romanov, V.A.
16 - Correlations between geochemical features of recent bottom and stream sediments in the Baikal geoecological polygon
In Koji Minoura, Editor , Lake Baikal Page 176-185 Publisher Elsevier Science B.V. , Amsterdam 2000 176-185
DOI:https://doi.org/10.1016/B978-044450434-0/50017-2
ISBN:
978-0-444-50434-0
127.
Kipfer, R.; Peeters, F.
24 - Some speculations on the possibility of changes in deep-water renewal in Lake Baikal and their consequences
In Koji Minoura, Editor , Lake Baikal Page 273-280 Publisher Elsevier Science B.V. , Amsterdam 2000 273-280
DOI:https://doi.org/10.1016/B978-044450434-0/50025-1
ISBN:
978-0-444-50434-0
126.
Takamatsu, T.; Kawai, T.; Nishikawa, M.
14 - Elemental composition of short sediment cores and ferromanganese concretions from Lake Baikal
In Koji Minoura, Editor , Lake Baikal Page 155-164 Publisher Elsevier Science B.V. , Amsterdam 2000 155-164
DOI:https://doi.org/10.1016/B978-044450434-0/50015-9
ISBN:
978-0-444-50434-0
125.
Ogawa, N.O.; Yoshii, K.; Melnik, N.G.; Bondarenko, N.A.; Timoshkin, O.A.; Smirnova-Zalumi, N.S.; Smirnov, V.V.; Wada, E.
23 - Carbon and nitrogen isotope studies of the pelagic ecosystem and environmental fluctuations of lake baikal
In Koji Minoura, Editor , Lake Baikal Page 262-272 Publisher Elsevier Science B.V. , Amsterdam 2000 262-272
DOI:https://doi.org/10.1016/B978-044450434-0/50024-X
ISBN:
978-0-444-50434-0
124.
Martens, K.; Schön, I.
29 - The importance of habitat stability for the prevalence of sexual reproduction
In Koji Minoura, Editor , Lake Baikal Page 324-330 Publisher Elsevier Science B.V. , Amsterdam 2000 324-330
DOI:https://doi.org/10.1016/B978-044450434-0/50030-5
ISBN:
978-0-444-50434-0
123.
Nakata, H.; Tanabe, S.; Iwata, H.; Amano, M.; Miyazaki, N.; Petrov, E.A.; Tatsukawa, R.
25 - Contamination of the ecosystems of lake baikal by persistent organochlorines
In Koji Minoura, Editor , Lake Baikal Page 281-298 Publisher Elsevier Science B.V. , Amsterdam 2000 281-298
DOI:https://doi.org/10.1016/B978-044450434-0/50026-3
ISBN:
978-0-444-50434-0
122.
Mashiko, K.; Kamaltynov, R.; Morino, H.; Sherbakov, D.Yu.
26 - Genetic differentiation of gammarid (Eulimnogammarus cyaneus) populations in relation to past environmental changes in lake baikal
In Koji Minoura, Editor , Lake Baikal Page 299-305 Publisher Elsevier Science B.V. , Amsterdam 2000 299-305
DOI:https://doi.org/10.1016/B978-044450434-0/50027-5
ISBN:
978-0-444-50434-0
121.
Yabe, M.; Sideleva, V.G.
27 - Myological peculiarities of the comephoridae: An endemic fish taxon in Lake Baikal (Pisces: Teleostei)
In Koji Minoura, Editor , Lake Baikal Page 306-314 Publisher Elsevier Science B.V. , Amsterdam 2000 306-314
DOI:https://doi.org/10.1016/B978-044450434-0/50028-7
ISBN:
978-0-444-50434-0
120.
Amano, M.; Koyama, Y.; Petrov, E.A.; Hayano, A.; Miyazaki, N.
28 - Morphometric comparison of skulls of seals of the subgenus Pusa
In Koji Minoura, Editor , Lake Baikal Page 315-323 Publisher Elsevier Science B.V. , Amsterdam 2000 315-323
DOI:https://doi.org/10.1016/B978-044450434-0/50029-9
ISBN:
978-0-444-50434-0
119.
Sakai, H.; Nomura, S.; Horii, M.; Kashiwaya, K.; Tanaka, A.; Kawai, T.; Kravchinsky, V.; Peck, J.
3 - Paleomagnetic and rock-magnetic studies on lake baikal sediments -BDP96 borehole at academician ridge-
In Koji Minoura, Editor , Lake Baikal Page 35-52 Publisher Elsevier Science B.V. , Amsterdam 2000 35-52
DOI:https://doi.org/10.1016/B978-044450434-0/50004-4
ISBN:
978-0-444-50434-0
118.
Kashiwaya, K.; Tanaka, A.; Sakai, H.; Kawai, T.
4 - Paleoclimatic signals printed in lake baikal sediments
In Koji Minoura, Editor , Lake Baikal Page 53-70 Publisher Elsevier Science B.V. , Amsterdam 2000 53-70
DOI:https://doi.org/10.1016/B978-044450434-0/50005-6
ISBN:
978-0-444-50434-0
117.
Karabanov, E.B.; Kuzmin, M.I.; Prokopenko, A.A.; Williams, D.F.; Khursevich, G.K.; Bezrukova, E.V.; Kerber, E.V.; N.}, Gvozdkov {A.; F.}, Gelety {V.; D., Weil; M., Schwab
5 - Glaciations of central asia in the late cenozoic according to the sedimentary record from lake baikal
In Koji Minoura, Editor , Lake Baikal Page 71-84 Publisher Elsevier Science B.V. , Amsterdam 2000 71-84
DOI:https://doi.org/10.1016/B978-044450434-0/50006-8
ISBN:
978-0-444-50434-0
116.
Demske, D.; Mohr, B.; Oberhänsli, H.
6 - Palaeoclimatic changes from 3.6 to 2.2 ma b.p. derived from palynological studies on lake baikal sediments
In Koji Minoura, Editor , Lake Baikal Page 85-89 Publisher Elsevier Science B.V. , Amsterdam 2000 85-89
DOI:https://doi.org/10.1016/B978-044450434-0/50007-X
ISBN:
978-0-444-50434-0
115.
Müller, J.; Kasbohm, J.; Oberhänsli, H.; Melles, M.; Hubberten, H.W.
7 - TEM analysis of smectite-illite mixed-layer minerals of core BDP 96 hole 1: Preliminary results
In Koji Minoura, Editor , Lake Baikal Page 90-100 Publisher Elsevier Science B.V. , Amsterdam 2000 90-100
DOI:https://doi.org/10.1016/B978-044450434-0/50008-1
ISBN:
978-0-444-50434-0
114.
Kawamuro, K.; Shichi, K.; Hase, Y.; Iwauchi, A.; Minoura, K.; Oda, T.; Takahara, H.; Sakai, H.; Morita, Y.; Miyoshi, N.; Kuzmin, M.I.
8 - Forest-desert alternation history revealed by the pollen-record in lake baikal over the past 5 million years
In Koji Minoura, Editor , Lake Baikal Page 101-107 Publisher Elsevier Science B.V. , Amsterdam 2000 101-107
DOI:https://doi.org/10.1016/B978-044450434-0/50009-3
ISBN:
978-0-444-50434-0
113.
Takahara, H.; Krivonogov, S.K.; Bezrukova, E.V.; Miyoshi, N.; Morita, Y.; Nakamura, T.; Hase, Y.; Shinomiya, Y; Kawamuro, K.
9 - Vegetation history of the southeastern and eastern coasts of Lake Baikal from bog sediments since the last interstade
In Koji Minoura, Editor , Lake Baikal Page 108-118 Publisher Elsevier Science B.V. , Amsterdam 2000 108-118
DOI:https://doi.org/10.1016/B978-044450434-0/50010-X
ISBN:
978-0-444-50434-0
112.
Eckert, C.; Veinberg, E.V.; Kienel, U.; Oberhänsli, H.
12 - A new preparation method for qualitative and quantitative analysis of fossil sponge spicules by light microscopy
In Koji Minoura, Editor , Lake Baikal Page 136-145 Publisher Elsevier Science B.V. , Amsterdam 2000 136-145
DOI:https://doi.org/10.1016/B978-044450434-0/50013-5
ISBN:
978-0-444-50434-0
111.
Khursevich, G.K.; Karabanov, E.B.; Williams, D.F.; Kuzmin, M.I.; Prokopenko, A.A.
13 - Evolution of freshwater centric diatoms within the Baikal rift zone during the late Cenozoic
In Koji Minoura, Editor , Lake Baikal Page 146-154 Publisher Elsevier Science B.V. , Amsterdam 2000 146-154
DOI:https://doi.org/10.1016/B978-044450434-0/50014-7
ISBN:
978-0-444-50434-0
110.
Mats, V.D.; Fujii, S.; Mashiko, K.; Osipov, E.Yu.; Yefrimova, I.M.; Klimansky, A.V.
2 - Changes in lake baikal water levels and runoff direction in the quaternary period
In Koji Minoura, Editor , Lake Baikal Page 15-34 Publisher Elsevier Science B.V. , Amsterdam 2000 15-34
DOI:https://doi.org/10.1016/B978-044450434-0/50003-2
ISBN:
978-0-444-50434-0
109.
Takamatsu, N.; Matsumoto, I.G.; Kato, N.; Kawai, T.
11 - Paleoenvironmental changes in the Eurasian continent interior inferred from chemical elements in sediment cores (BDP96/1, BDP96/2) from Lake Baikal
In Koji Minoura, Editor , Lake Baikal Page 127-135 Publisher Elsevier Science B.V. , Amsterdam 2000 127-135
DOI:https://doi.org/10.1016/B978-044450434-0/50012-3
ISBN:
978-0-444-50434-0
108.
Mapping the Hawaiian plume conduit with converted seismic waves
Li, X.; Kind, R.; Priestloy, K.; Sobolev, S.V.; Tilmann, F.; Yuar, X.; Weber, M.
Nature, 405 (6789) 938-941 2000
ISSN: 00280836
DOI:10.1038/35016054
Keywords:▾ crustal structure; hot spot; mantle plume; seismic velocity, air temperature; article; atmosphere; geography; plume; priority journal; sea; shear rate; United States; volcano, Pacific Ocean
Abstract: ▾ The volcanic edifice of the Hawaiian islands and seamounts, as well as the surrounding area of shallow sea floor known as the Hawaiian swell, are believed to result from the passage of the oceanic lithosphere over a mantle hotspot. Although geochemical and gravity observations indicate the existence of a mantle thermal plume beneath Hawaii, no direct seismic evidence for such a plume in the upper mantle has yet been found. Here we present an analysis of compressional-to-shear (P-to-S) converted seismic phases, recorded on seismograph stations on the Hawaiian islands, that indicate a zone of very low shear-wave velocity (< 4 km s-1) starting at 130-140 km depth beneath the central part of the island of Hawaii and extending deeper into the upper mantle. We also find that the upper-mantle transition zone (410-660 km depth) appears to be thinned by up to 40-50 km to the south-southwest of the island of Hawaii. We interpret these observations as localized effects of the Hawaiian plume conduit in the asthenosphere and mantle transition zone with excess temperature of ~300°C. Large variations in the transition-zone thickness suggest a lower-mantle origin of the Hawaiian plume similar to the Iceland plume, but our results indicate a 100°C higher temperature for the Hawaiian plume.
107.
Matsumoto, G.I.; Kosaku, S.; Takamatsu, N.; Akagi, T.; Kawai, T.; Ambe, Y.
10 - Estimation of paleoenvironmental changes in the Eurasian continental interior during the past 5 million years inferred from organic components in the BDP96 1
In Koji Minoura, Editor , Lake Baikal Page 119-126 Publisher Elsevier Science B.V. , Amsterdam 2000 119-126
DOI:https://doi.org/10.1016/B978-044450434-0/50011-1
ISBN:
978-0-444-50434-0
106.
A new estimate of the Holocene lowstand level of Lake Titicaca, central Andes, and implications for tropical palaeohydrology
Cross, Scott L.; Baker, Paul A.; Seltzer, Geoffrey O.; Fritz, Sherilyn C.; Dunbar, Robert B.
Holocene, 10 (1) 21 – 32 2000
DOI:10.1191/095968300671452546
Keywords:▾ Bolivia; Lake Titicaca; Holocene; lake level; lowstand; paleohydrology
Abstract: ▾ New evidence from piston cores and high-resolution seismic reflection data shows that water levels in Lake Titicaca were as much as 100 m below the present level during the early to mid-Holocene (between >6 and 3.8 14C kyr BP). Climatological and modelling studies indicate that Lake Titicaca rainfall depends on convective activity in upwind Amazonia; the lake-level data therefore suggest a drier Amazon Basin during this time. This view is bolstered by an excellent match between the Titicaca lake-level curve and decreased methane concentrations in Greenland ice, previously ascribed to drying of low-latitude wetlands (Blunier et al., 1995). The postglacial history of Lake Titicaca fits a global pattern of lake-level change in the tropics, characterized by opposite phasing between the Southern and Northern Hemispheres. This pattern is most likely the result of orbital controls over the intensity of summer insolation.
105.
A new record of Holocene climate change from the bottom sediments of Lake Baikal
Karabanov, E.B.; Prokopenko, A.A.; Williams, D.F.; Khursevich, G.K.
Palaeogeography, Palaeoclimatology, Palaeoecology, 156 (3-4) 211 – 224 2000
DOI:10.1016/S0031-0182(99)00141-8
104.
Clay minerals in bottom sediments of Lake Baikal as indicators of climate change
Kuz'min, M.I.; Solotchina, E.P.; Vasilevskii, A.N.; Stolpovskaya, V.N.; Karabanov, E.B.; Geletii, V.F.; Bychinskii, V.A.; Anoshin, G.N.; Shul'zhenko, S.G.
Geologiya i Geofizika, 41 (10) 1347 – 1359 2000
ISSN: 00167886
Abstract: ▾ The mineral assemblage of Pliocene - Pleistocene bottom sediments of Lake Baikal, exposed by the deep-sea BDP-96-2 (Baikal Drilling Project) has been studied by the methods of XRD and IR spectroscopy. Complex XRD patterns of clay minerals have been modeled using an advanced algorithm based on calculation of interference function from one-dimensional disordered crystals of finite thickness. The modeling implies fitting of theoretical to observed patterns and optimization procedure by methods of nonlinear programming. It has been shown that major clay minerals in the sediments that formed for the past 2.5 Ma during cold stages are illite-illite-smectites with predominantly illite layers, and chlorite; the principal clay minerals in the sediments that formed during warm periods are smectite, illite-smectites with high contents of smectite layers, and chlorite-smectites. These data allow unravelling the climate history of Lake Baikal from biogenic silica record.