Geologos 25, 2 (2019): 175–179
DOI: 10.2478/logos-2019-0016
The First International Conference on ‘Processes
and Palaeo-Environmental Changes in the Arctic:
From Past to Present’ (PalaeoArc)
Astrid Lyså1*, ĺvar Örn Benediktsson2, Andy Emery3, Lauren Gregoire3,
Anne Jennings4, Caterina Morigi5, Juliane Müller6, Matt O´Regan7,
Pertti Sarala8, Chris Stokes9, Witold Szczuciński10, Monica Winsborrow11
1
Geological Survey of Norway, Norway,
2
University of Iceland, Iceland,
3
University of Leeds, UK,
4
INSTAAR, University of Colorado, USA,
5
University of Pisa, Italy,
6
Alfred Wegner Institute, Germany,
7
Stockholm University, Stockholm,
8
Oulu Mining School, University of Oulu, Finland,
9
Durham University, UK,
10
Adam Mickiewicz University in Poznań, Poland,
11
The Arctic University of Norway in Tromsø, Norway
*corresponding author: e-mail:
[email protected]
The new international network PalaeoArc (Processes and Palaeo-Environmental Changes in the
Arctic: From Past to Present) held its first meeting
in Poznań, 20–24 May 2019. The meeting was hosted by the Faculty of Geographical and Geological
Sciences, Adam Mickiewicz University, Poznań,
and organized by a local committee chaired by Witold Szczuciński.
PalaeoArc is an international research programme network which aims to understand and
explain the climatically induced environmental changes in the Arctic that have taken place
throughout the Quaternary and continue to the
present-day. The network was established in 2018,
building on and extending the rich legacy of the
previous network programmes that include PAST
Gateways (Palaeo-Arctic Spatial and Temporal
Gateways), APEX (Arctic Palaeoclimate and its Extremes), QUEEN (Quaternary Environment of the
Eurasian North) and PONAM (Polar North Atlantic
Margins – Late Cenozoic Evolution). There are four
major themes of the programme: 1) the dynamics of
the Arctic ice sheets, ice shelves and glaciers; 2) the
dynamics of high latitude oceans and sea ice; 3) the
dynamics of the terrestrial environment and landscape evolution; and 4) the climatic response to,
and interaction between, these different parts of the
Arctic system. As a research network, PalaeoArc
strives to bring together and build bridges between
scientists from different countries and career stages,
and from different disciplines in Arctic science. This
includes marine and terrestrial researchers working
with empirical data or numerical modelling. A key
focus of the network’s activities is an annual international conference that brings together Arctic scientists from a number of disciplines and typically
includes an excursion.
The first PalaeoArc annual meeting held in
Poznań was attended by 69 participants from 11
countries (Fig. 1). Enthusiastic participants, the ex-
176
Astrid Lyså et al.
Fig. 1. Participants of The First International Conference ´Processes and Palaeo-Environmental changes in the Arctic:
From Past to Present´ (PalaeoArc). Photo by Sz. Belzyt
cellent organization of the conference, and an exciting and well-planned field trip, made the meeting a
great success.
The meeting started on Monday May 20th with
registration at the Institute of Geology, Faculty of Geographical and Geological Sciences. Three different
workshops were held for preregistered users. These
workshops were 1) Hands-on dendrochronology (led
by Agata Buchwał and Pawel Matulewski), 2) AMS
14
C Laboratory visit (led by Karina Apolinarska and
Tomasz Goslar) and 3) Poland – a unique place to fund
and run innovative and challenging research projects for
young scientists (led by Mateusz Strzelecki). The first
day ended with a fantastic outdoor icebreaker and
BBQ that facilitated a reunion of researchers and the
opportunity to get to know new ones.
The conference was officially opened on Day 2
by Witold Szczuciński (Chair of the local organiz-
ing committee), Błażej Berkowski (Director of the
Institute of Geology) and Astrid Lyså (Chair of
PalaeoArc). A total of 17 speakers, including two
keynote talks, presented new scientific results from
the study of former ice sheets, ice-sheet dynamics,
oceans, and sea ice in the Arctic. The outstanding
keynotes by Kurt H. Kjær (A large impact crater beneath Hiawatha Glacier in northwest Greenland, Kjær
et al., 2019) and Karl Stattegger (Sea-level change and
the role of polar ice sheets, Stattegger, 2019) provided
an excellent framework for the scientific topics and
stimulated many fruitful discussions that continued during the refreshment breaks. At the end of
the day, 27 posters were presented, eight of these
by early carrier researchers competing for the best
poster award.
The field trip on Day 3 was organized by Izabela Szuman-Kalita, Marek Ewertowski, Jakub
Fig. 2. Witold Szczuciński
presents the story behind
the impact craters at the
Morasko Meteorite Nature
Reserve. One of the water-filled craters is visible
in the background. Photo
by A. Emery
The First International Conference on ‘Processes and Palaeo-Environmental Changes in the Arctic: From Past to Present’
177
Kalita, Leszek Kasprzak, Mirosław Makohonienko,
Krzysztof Pleskot, Witold Szczuciński and Aleksandra Tomczyk. The conference group was introduced to fascinating and exciting geological localities related to the last Scandinavian Ice Sheet in
Wielkopolska and Mid-Holocene meteorite impact
craters. Excellent guiding and engaged discussions
among the participants reminded us that a field excursion is very important for gathering researchers
and creating a friendly, constructive and open atmosphere among scientists.
Three sites were visited, the first of which was
the Morasko Meteorite Nature Reserve (Fig. 2). The
participants were introduced to meteorite craters
superimposed on a belt of recessional moraines that
were formed around 18,500 years ago, during the
Poznań phase of the last glaciation (Karczewski,
1976; Chmal, 1990; Kozarski, 1995; Stankowski,
2001, 2008). Impressive amounts of data have been
collected and published over many years, leading
to the interpretation of the depressions as impact
craters, which were likely to have been formed
around 5000-5500 years ago. This is largely based
on environmental studies of sediments at the crater rim and from lake sediments close to the craters
(e.g., Szczuciński et al., 2016; Pleskot et al., 2018;
Szokaluk et al., 2019). Studies of meteorites related
to this event have resulted in the discovery of two
new minerals, moraskoite (Karwowski et al., 2015)
and czochralskiite (Karwowski et al., 2016).
Site 2, where glaciofluvial sand and esker sediments near Tomice were visited, was in an interstream zone between ice streams at the foreland of
the Poznań phase. At this site, diamicton occurred
at the surface, and complicated deformation structures were visible in the underlying sediments. Permafrost-related structures were observed, as well
as loading structures and glaciotectonised deformation structures, such as recumbent folds and thrust
planes. Large-scaled glaciotectonic structures were
also visible at Site 3, the Kuślin site, which is located
near to ice-marginal position (Fig. 3). In contrast to
Site 2, subglacial till was not observed at the surface
of Site 3, with glaciotectonised stratigraphy truncated by a planar surface, onto which Holocene and
recent soils were deposited. Research on sedimentological and chronological analysis of this recently
discovered site is in progress. Both Sites 2 and 3 led
to many discussions and stimulated exchange of
ideas about the large variety of deformation structures and ice-stream behaviour.
The last two days of the conference comprised 22
talks and the final poster session. A further keynote
talk by Thomas Opel (Ice wedges: a powerful continental climate archive?, Opel et al., 2019) marked an interesting introduction to the terrestrial environment
and landscape evolution in the Arctic. This was the
perfect introduction to the PalaeoArc theme on the
climatic response to, and interaction between, the
different parts of the Arctic, which was the focus of
many of the talks over the last two days. As with
the first day of presentations, there were numerous
fruitful and interesting discussions.
A further highlight of a fantastic, well-organized, friendly and inspiring PalaeoArc conference
was the conference dinner at the Galeria Tumska
restaurant in Poznań on Day 4. During the dinner,
many speeches were given, including by Astrid
Lyså, the chair of the PalaeoArc Steering Committee, who thanked the local organization committee
and the field guides for the effort and the excellent
work behind the entire conference event. A further
highlight was the speech by Professor Emeritus Jan
Mangerud (Fig. 4), the internationally renowned
Fig. 3. Large-scaled glaciotectonic deformation at the
Kuślin site. Photo by A. Lyså
Fig. 4. Jan Mangerud giving a speech at the conference
dinner. Photo by A. Emery
178
Astrid Lyså et al.
glacial geologist, who was one of the initiators of
the first PONAM network in the late 1980s. In addition to several entertaining anecdotes, he emphasized the importance that this type of network has
in gathering researchers at different career stages.
As the PalaeoArc network aims to build bridges between researchers at different career levels, students
were encouraged to give poster presentation during the conference. The PalaeoArc steering committee selected a ‘best poster’ from the many interesting student posters. During the dinner, the winner
was announced. The prize which was a certificate
accompanied by a book about Poland, was handed
over to the winner, Bor-Jiun Jong, by Andy Emery,
the young scientists’ representative on the PalaeoArc steering committee (Fig. 5). Bor-Jiun is from
the National Taiwan University, and was awarded
the prize for the poster entitled ‘Ba/Ca ratios and oxygen isotopic composition of planktonic foraminifera in
the Arctic Ocean as a tool for reconstructing paleo-river-
ine freshwater input’, which was presented together
with co-authors Ludvig Löwemark and Chih-Kai
Chuang.
Before closing the PalaeoArc First International
Conference, the steering committee announced that
the PalaeoArc Second International Conference will
be held in Pisa, Italy, on 25-29 May 2020. Caterina
Morigi, at the University in Pisa, will be chair of the
local organising committee.
Acknowledgements
The organisers are thanked for a very well-organized conference and field trip, and for introducing
the PalaeoArc community to the exciting and interesting glacial geology close to the Weichselian
ice sheet margin in Wielkopolska, and the impact
craters in the Morasko Meteorite Nature Reserve.
Members of the local organizing committee were
Witold Szczuciński (chair), Krzysztof Pleskot (secretary), Karina Apolinarska, Agata Buchwał, Marek
Ewertowski, Leszek Kasprzak, Karolina Leszczyńska, Mirosław Makohonienko, Jakub Małecki,
Krzysztof Rymer, Mateusz Strzelecki, Izabela Szuman-Kalita and Paweł Wolniewicz. All the participants of the conference are warmly thanked for inspiring presentations and for engaging discussions
around PalaeoArc’s key themes. The Dean of the
Faculty of Geographical and Geological Sciences,
Professor Leszek Kasprzak is thanked for financial
support to the meeting.
Additional material
Book of abstracts: http://palaeoarc.amu.edu.pl/wp-content/uploads/2019/05/PaleoArctic-Abstracts.pdf
Field trip guide: http://palaeoarc.amu.edu.pl/wp-content/uploads/2019/05/PaleoArctic-Guide.pdf
Twitter: https://twitter.com/PalaeoArc
PalaeoArc website: http://www.palaeoarc.no/
Interview with Prof. Jan Mangerud
https://glacjoblogia.wordpress.com/2019/05/25/rozmowa-prof-jan-mangerud-bez-ciekawosci-nie-bedziesz-dobrym-naukowcem/
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Fig. 5. The prize for the best student poster was handed
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PalaeoArc steering committee student representative
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