TY  - JOUR
A1  - Arnison, Paul G.
A1  - Bibb, Mervyn J.
A1  - Bierbaum, Gabriele
A1  - Bowers, Albert A.
A1  - Bugni, Tim S.
A1  - Bulaj, Grzegorz
A1  - Camarero, Julio A.
A1  - Campopiano, Dominic J.
A1  - Challis, Gregory L.
A1  - Clardy, Jon
A1  - Cotter, Paul D.
A1  - Craik, David J.
A1  - Dawson, Michael
A1  - Dittmann-Thünemann, Elke
A1  - Donadio, Stefano
A1  - Dorrestein, Pieter C.
A1  - Entian, Karl-Dieter
A1  - Fischbach, Michael A.
A1  - Garavelli, John S.
A1  - Goeransson, Ulf
A1  - Gruber, Christian W.
A1  - Haft, Daniel H.
A1  - Hemscheidt, Thomas K.
A1  - Hertweck, Christian
A1  - Hill, Colin
A1  - Horswill, Alexander R.
A1  - Jaspars, Marcel
A1  - Kelly, Wendy L.
A1  - Klinman, Judith P.
A1  - Kuipers, Oscar P.
A1  - Link, A. James
A1  - Liu, Wen
A1  - Marahiel, Mohamed A.
A1  - Mitchell, Douglas A.
A1  - Moll, Gert N.
A1  - Moore, Bradley S.
A1  - Mueller, Rolf
A1  - Nair, Satish K.
A1  - Nes, Ingolf F.
A1  - Norris, Gillian E.
A1  - Olivera, Baldomero M.
A1  - Onaka, Hiroyasu
A1  - Patchett, Mark L.
A1  - Piel, Jörn
A1  - Reaney, Martin J. T.
A1  - Rebuffat, Sylvie
A1  - Ross, R. Paul
A1  - Sahl, Hans-Georg
A1  - Schmidt, Eric W.
A1  - Selsted, Michael E.
A1  - Severinov, Konstantin
A1  - Shen, Ben
A1  - Sivonen, Kaarina
A1  - Smith, Leif
A1  - Stein, Torsten
A1  - Suessmuth, Roderich D.
A1  - Tagg, John R.
A1  - Tang, Gong-Li
A1  - Truman, Andrew W.
A1  - Vederas, John C.
A1  - Walsh, Christopher T.
A1  - Walton, Jonathan D.
A1  - Wenzel, Silke C.
A1  - Willey, Joanne M.
A1  - van der Donk, Wilfred A.
T1  - Ribosomally synthesized and post-translationally modified peptide natural products overview and recommendations for a universal nomenclature
JF  - Natural product reports : a journal of current developments in bio-organic chemistry
N2  - This review presents recommended nomenclature for the biosynthesis of ribosomally synthesized and post-translationally modified peptides (RiPPs), a rapidly growing class of natural products. The current knowledge regarding the biosynthesis of the >20 distinct compound classes is also reviewed, and commonalities are discussed.
Y1  - 2013
U6  - https://doi.org/10.1039/c2np20085f
SN  - 0265-0568
VL  - 30
IS  - 1
SP  - 108
EP  - 160
PB  - Royal Society of Chemistry
CY  - Cambridge
ER  - 
TY  - JOUR
A1  - Stroeven, Arjen P.
A1  - Hättestrand, Clas
A1  - Kleman, Johan
A1  - Heyman, Jakob
A1  - Fabel, Derek
A1  - Fredin, Ola
A1  - Goodfellow, Bradley W.
A1  - Harbor, Jonathan M.
A1  - Jansen, John D.
A1  - Olsen, Lars
A1  - Caffee, Marc W.
A1  - Fink, David
A1  - Lundqvist, Jan
A1  - Rosqvist, Gunhild C.
A1  - Stromberg, Bo
A1  - Jansson, Krister N.
T1  - Deglaciation of Fennoscandia
JF  - Quaternary science reviews : the international multidisciplinary research and review journal
N2  - To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and geochronological data from radiocarbon, varve, optically-stimulated luminescence, and cosmogenic nuclide dating. This is summarized as a deglaciation map of the Fennoscandian Ice Sheet with isochrons marking every 1000 years between 22 and 13 cal kyr BP and every hundred years between 11.6 and final ice decay after 9.7 cal kyr BP. Deglaciation patterns vary across the Fennoscandian Ice Sheet domain, reflecting differences in climatic and geomorphic settings as well as ice sheet basal thermal conditions and terrestrial versus marine margins. For example, the ice sheet margin in the high-precipitation coastal setting of the western sector responded sensitively to climatic variations leaving a detailed record of prominent moraines and other ice-marginal deposits in many fjords and coastal valleys. Retreat rates across the southern sector differed between slow retreat of the terrestrial margin in western and southern Sweden and rapid retreat of the calving ice margin in the Baltic Basin. Our reconstruction is consistent with much of the published research. However, the synthesis of a large amount of existing and new data support refined reconstructions in some areas. For example, the LGM extent of the ice sheet in northwestern Russia was located far east and it occurred at a later time than the rest of the ice sheet, at around 17-15 cal kyr BP. We also propose a slightly different chronology of moraine formation over southern Sweden based on improved correlations of moraine segments using new LiDAR data and tying the timing of moraine formation to Greenland ice core cold stages. Retreat rates vary by as much as an order of magnitude in different sectors of the ice sheet, with the lowest rates on the high-elevation and maritime Norwegian margin. Retreat rates compared to the climatic information provided by the Greenland ice core record show a general correspondence between retreat rate and climatic forcing, although a close match between retreat rate and climate is unlikely because of other controls, such as topography and marine versus terrestrial margins. Overall, the time slice reconstructions of Fennoscandian Ice Sheet deglaciation from 22 to 9.7 cal kyr BP provide an important dataset for understanding the contexts that underpin spatial and temporal patterns in retreat of the Fennoscandian Ice Sheet, and are an important resource for testing and refining ice sheet models. (C) 2015 The Authors. Published by Elsevier Ltd.
KW  - Fennoscandian Ice Sheet
KW  - Deglaciation
KW  - Glacial geomorphology
KW  - Geochronology
KW  - Ice sheet dynamics
Y1  - 2016
U6  - https://doi.org/10.1016/j.quascirev.2015.09.016
SN  - 0277-3791
VL  - 147
SP  - 91
EP  - 121
PB  - Elsevier
CY  - Oxford
ER  - 
TY  - JOUR
A1  - Markovic, Danijela
A1  - Carrizo, Savrina F.
A1  - Kaercher, Oskar
A1  - Walz, Ariane
A1  - David, Jonathan N. W.
T1  - Vulnerability of European freshwater catchments to climate change
JF  - Global change biology
N2  - Climate change is expected to exacerbate the current threats to freshwater ecosystems, yet multifaceted studies on the potential impacts of climate change on freshwater biodiversity at scales that inform management planning are lacking. The aim of this study was to fill this void through the development of a novel framework for assessing climate change vulnerability tailored to freshwater ecosystems. The three dimensions of climate change vulnerability are as follows: (i) exposure to climate change, (ii) sensitivity to altered environmental conditions and (iii) resilience potential. Our vulnerability framework includes 1685 freshwater species of plants, fishes, molluscs, odonates, amphibians, crayfish and turtles alongside key features within and between catchments, such as topography and connectivity. Several methodologies were used to combine these dimensions across a variety of future climate change models and scenarios. The resulting indices were overlaid to assess the vulnerability of European freshwater ecosystems at the catchment scale (18 783 catchments). The Balkan Lakes Ohrid and Prespa and Mediterranean islands emerge as most vulnerable to climate change. For the 2030s, we showed a consensus among the applied methods whereby up to 573 lake and river catchments are highly vulnerable to climate change. The anthropogenic disruption of hydrological habitat connectivity by dams is the major factor reducing climate change resilience. A gap analysis demonstrated that the current European protected area network covers <25% of the most vulnerable catchments. Practical steps need to be taken to ensure the persistence of freshwater biodiversity under climate change. Priority should be placed on enhancing stakeholder cooperation at the major basin scale towards preventing further degradation of freshwater ecosystems and maintaining connectivity among catchments. The catchments identified as most vulnerable to climate change provide preliminary targets for development of climate change conservation management and mitigation strategies.
KW  - catchment connectivity
KW  - climate change
KW  - exposure
KW  - freshwater biodiversity
KW  - gap analysis
KW  - resilience
KW  - sensitivity
KW  - vulnerability
Y1  - 2017
U6  - https://doi.org/10.1111/gcb.13657
SN  - 1354-1013
SN  - 1365-2486
VL  - 23
SP  - 3567
EP  - 3580
PB  - Wiley
CY  - Hoboken
ER  -