Re: New Research Topic at Frontiers

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Re: New Research Topic at Frontiers

Evgeniya Kandiano
Dear everybody,


We cordially invite you to submit a paper to our “Research Topic” in Frontiers in Earth Science. For this special issue, we aim to compile a collection of articles devoted to the topic “Paleoceanographic Conditions in High Northern Latitudes during Quaternary Interglaciations” (see abstract below). We expect our “Research Topic” to include papers based on various sedimentological, faunal and (organic) geochemical methods. Please note that the journal is willing to assist with removing any barrier to publishing and has developed solutions regarding publishing fees, including numerous institutional agreements that cover the publishing costs, as well as waivers for those without funding. For more information on these solutions, please click here: https://www.frontiersin.org/research-topics/7003/paleoceanographic-conditions-in-high-northern-latitudes-during-quaternary-interglaciations

What advantages will you have when publishing your paper in our Research Topic?

Manuscripts published in Research Topics have higher visibility and have a trend for higher citations compared to solo submissions;

All Frontiers in Earth Science articles are fully Gold Open Access with a CC-BY license, so authors retain the copyright to their articles;

Frontiers in Earth Science upload articles online as soon as they are accepted for publication without any embargo period;

Our “Research Topic” has its own dedicated web page: Paleoceanographic Conditions in High Northern Latitudes during Quaternary Interglaciations;

Participation in a Frontiers “Research Topic” helps to engage the community and stimulate discussion;

There is opportunity to publish articles in a free Gold Open Access eBook;

Our “Research Topic” is being announced simultaneously through three popular sections of the Frontiers Earth in Science journal: Biogeochemistry, Geochemistry, and Quaternary Science, Geomorphology and Paleoenvironment which will attract more attention to its publications.

How to proceed with submitting a paper?

Please notify us vie email ([hidden email]) about your intention to write a paper for our “Research Topic”;

Submit your abstract before 01.02.2018 through the “Research Topic” web page Paleoceanographic Conditions in High Northern Latitudes during Quaternary Interglaciations;

Submit your paper before 28.07.2018 through the “Research Topic” web page Paleoceanographic Conditions in High Northern Latitudes during Quaternary Interglaciations.


With best regards,


The editors
Evgenia Kandiano
Thomas Cronin 
Kirstin Werner
Juliane Müller


Abstract:


Current climate warming is dramatically amplified in high latitudes of the Northern Hemisphere, notably through sea-ice retreat and melting of the Greenland ice sheet. These processes, in turn, trigger feedback mechanisms affecting ocean temperature and circulation. These oceanographic mechanisms and interactions with sea ice, the atmosphere and adjacent land areas need to be investigated in order to understand the extent and further development of the ongoing climate change.

Paleoceanographic reconstructions of past interglacial periods in high northern latitudes can provide useful insights and scenarios for future climate prediction. However, such reconstructions in subpolar and polar environments involve multiple challenges due to a strong influence of melt water, quantifying temperature calibrations, restricted species’ compositions in many biological groups, and others. Significant recent advances in developing new paleoceanographic methods (especially in the field of geochemistry and biogeochemistry) and elaborating existing methods allow for evaluation of past changes in seasonal sea-ice extent, salinity, and ocean circulation. Paleo-temperature estimations of surface, subsurface and bottom waters also have been considerably improved.

In this Research Topic, we welcome contributions exploring oceanic environments in high northern latitudes during the pronounced Quaternary interglacial periods, especially Marine Isotope Stages 11, 9, 5e, and 1, by means of various paleoceanographical methods, from paleontological to biogeochemical. Suborbital and millennial-scale reconstructions of oceanic conditions and circulation are especially encouraged.




************************************************


Dr. Evgenia S. Kandiano

Helmholtz-Zentrum für Ozeanforschung Kiel 
Wischhofstr. 1-3, Geb.4, Raum 305
24148 Kiel, Germany

Tel.: +49 431 600-2848<img class="\22skype_c2c_logo_img\22" height="\220\22" width="\220\22" pnsrc="\22resource://skype_ff_extension-at-jetpack/skype_ff_extension/data/call_skype_logo.png\22" src="\22resource://skype_ff_extension-at-jetpack/skype_ff_extension/data/call_skype_logo.png\22">
Fax: +49 431 600-2961
E-mail: [hidden email]



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