IGCP Board; 10th session; Report of the ... - unesdoc - Unesco
IGCP Board; 10th session; Report of the ... - unesdoc - Unesco
IGCP Board; 10th session; Report of the ... - unesdoc - Unesco
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Summary <strong>of</strong> activities. The following international<br />
meetings have been arranged and attended.<br />
(a) A joint meeting <strong>of</strong> Project 158 and Holocene<br />
Eurosiberian Subcommission <strong>of</strong> INQUA, <strong>the</strong><br />
Symposium on "Palaeohydrology <strong>of</strong> <strong>the</strong> temperate<br />
zone" (Poznan, Poland, 22-28 September,<br />
1981) was organized by Pr<strong>of</strong>essors. Kozarski<br />
and A. Witt (Secretary), Adam Mickiewicz<br />
University in Poznañ and <strong>the</strong> Committee for<br />
Quaternary Research, Polish Academy <strong>of</strong> Sciences<br />
and attended by 37 foreign participants from<br />
15 countries and 38 from Poland. Thirty-five<br />
papers were presented during <strong>the</strong> meeting, mostly<br />
national reports. Some invited speakers presented<br />
<strong>the</strong> ways <strong>of</strong> palaeoecological, palaeohydrological,<br />
and palaeoclimatic reconstructions<br />
based on different evidence from fluvial, lake,<br />
and mire environments (T. Webb, N. Hotinsky,<br />
B. Berglund, L. Starkel, B. Frenzel, K.D. Jager,<br />
V. Lozek and M. Geyh) and <strong>the</strong> impact <strong>of</strong><br />
man on <strong>the</strong> environment (K. Gregory, P, Moore).<br />
Ano<strong>the</strong>r 17 papers at <strong>the</strong> poster <strong>session</strong> mainly<br />
presented results from different lake reference<br />
sites or river systems in Poland.<br />
During a four-day field trip, organized mostly<br />
by <strong>the</strong> Poznañ team, led by S. Kozarski, complex<br />
methods <strong>of</strong> studies were presented, covering<br />
palaeochannel fills and fluvial history in <strong>the</strong><br />
Warta valley and later Biskupin archaeological<br />
site, Gacno Wielkie lake (M. Hjelmroos-Ericsson),<br />
mires and dunes with fossil forest in<br />
Slowiñski National Park (K. Tobolski) and<br />
Zarnowieckie lake (M. Latalowa).<br />
A volume with abstracts <strong>of</strong> papers and an excursion<br />
guidebook were edited by S. Kozarski. This<br />
meeting summarized <strong>the</strong> four-year activity and<br />
showed distinct progress both in regional studies<br />
and in general methods and palaeohydrological<br />
reconstructions. A Project business meeting<br />
was organized during <strong>the</strong> symposium.<br />
(b) The Project-sponsored meeting on <strong>the</strong> absolute<br />
and radiocarbon chronology <strong>of</strong> varves, icecores<br />
and Mid-Holocene tree-rings took place<br />
in London from 30 April-1 May 1981, organized<br />
by Dr. D.J. Schove. It was attended by 10 participants<br />
from 7 countries. The problems <strong>of</strong><br />
teleconnection, absolute chronology <strong>of</strong> <strong>the</strong> lateglacial,<br />
role <strong>of</strong> volcanic eruptions, sunspots,<br />
geomagnetic variations, and o<strong>the</strong>r matters were<br />
discussed, with examples from different parts<br />
<strong>of</strong> Europe and America. The proceedings edited<br />
by R. Fairbridge and D.J. Schove are expected<br />
to be published.<br />
(c) The International Palaeolimnological Conference<br />
was convened in Koli, South Finland<br />
from 1-8 September 1981 and was attended by<br />
about 150 participants, several <strong>of</strong> whom were<br />
connected with Subproject B. Reference sites<br />
from different countries were demonstrated as<br />
posters, as well as <strong>the</strong> Finnish project programme<br />
for Subproject B (Y. Vasari). M. Ralska-<br />
Jasiewiczowa, secretary <strong>of</strong> Subproject B, took<br />
part in this meeting.<br />
50<br />
Subproject A: Fluvial environment. The revised<br />
version <strong>of</strong> <strong>the</strong> Subproject guidebook was edited in<br />
November 1981 by J. Thornes and L. Starkel<br />
and published by Geo Abstracts in <strong>the</strong> Technical<br />
Bulletin <strong>of</strong> <strong>the</strong> British Geomorphological Research<br />
Group. This new version includes a new chapter<br />
on palaeohydrological reconstructions written by<br />
M. Church.<br />
Official working groups now have been organized<br />
in Canada, Czechoslovakia, Finland, UK, Hungary,<br />
Poland, Roumania, and Switzerland. Active<br />
teams, or individual scientists from Belgium,<br />
FRG, <strong>the</strong> USA, Italy, and <strong>the</strong> Ne<strong>the</strong>rlands, have<br />
joined <strong>the</strong> work. Ano<strong>the</strong>r group <strong>of</strong> countries<br />
(France, Austria, <strong>the</strong> Soviet Union, China, Spain,<br />
and Australia) shows an interest in <strong>the</strong> Subproject.<br />
At <strong>the</strong> meeting in Poznañ <strong>the</strong> results <strong>of</strong> most <strong>of</strong><br />
<strong>the</strong> collective work were presented. L. Koutaniami<br />
(Oulu, Finland) showed new results <strong>of</strong> <strong>the</strong><br />
generations <strong>of</strong> palaeochannels in <strong>the</strong> Oulanka valley.<br />
K. Gregory (Southampton, UK) presented<br />
<strong>the</strong> next volume with preliminary results <strong>of</strong> studies<br />
in <strong>the</strong> Severn valley. J. Rose (London) discussed<br />
<strong>the</strong> palaeohydrological variations in <strong>the</strong><br />
Gipping River Valley during <strong>the</strong> late glacial. The<br />
Polish team gave a wide review <strong>of</strong> work mostly in<br />
<strong>the</strong> Vistula River Basin (Es Niedziaikowska,<br />
K. Klimek, K. Mamakowa and L. Starkel, A. Szumawski,<br />
E. Wiániewski, A. Tomczak, E. Drozdowski,<br />
J.E. Mojski, W . Florek) and during <strong>the</strong><br />
excursion in <strong>the</strong> Warta River Valley (S. Kozarski,<br />
B. Antczak, P. Gonera, K. Tobolski, I. Okuniewska).<br />
A close co-operation with palynologists working<br />
in Subproject B should be stressed. The monograph<br />
from <strong>the</strong> Wisloka valley was <strong>of</strong>fered to all<br />
participants.<br />
J. Havlicek (Prague, Czechoslovakia) presented<br />
<strong>the</strong> results <strong>of</strong> work in <strong>the</strong> Morawa River Valley.<br />
A broad summary <strong>of</strong> palaeohydrological changes<br />
based on well-dated alluvial fills in <strong>the</strong> upper<br />
Main Valley was given by W . Schirmer (Dusseldorf,<br />
FRG). The beginning <strong>of</strong> studies in <strong>the</strong><br />
Tisza and Bodrog River Valleys with a wide view<br />
<strong>of</strong> <strong>the</strong> channel changes in <strong>the</strong> subsiding basin was<br />
presented by Z. Borsy (Hungary). Ch. Schlüchter<br />
(Zurich, Switzerland) showed <strong>the</strong> preliminary results<br />
<strong>of</strong> work in <strong>the</strong> Aar River Valley in <strong>the</strong> Alps<br />
and <strong>the</strong>ir foreland. I. Heyse (Gent, Belgium)<br />
discussed <strong>the</strong> evolution <strong>of</strong> Sceldtbasin Valley<br />
dammed by sand dunes. Of special value was <strong>the</strong><br />
syn<strong>the</strong>tic presentation <strong>of</strong> work in <strong>the</strong> small Scottish<br />
River Valley North Esk by I. Mairels (Aberdeen,<br />
UK) who made <strong>the</strong> approach <strong>of</strong> using statistical<br />
methods for full palaeohydrological reconstructions<br />
based on studies <strong>of</strong> palaeochannels and<br />
alluvial fills. In a summarizing paper L. Starkel<br />
underlined <strong>the</strong> typology <strong>of</strong> river valleys <strong>of</strong> <strong>the</strong><br />
temperate zone, <strong>the</strong> main model <strong>of</strong> turning from<br />
braided to meandering channels, <strong>the</strong> human impact<br />
(this problem was discussed in detail by K.<br />
Gregory) and <strong>the</strong> origin <strong>of</strong> many fills side-by-side<br />
related to minor hydrological fluctuations.