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@@ -416,5 +416,122 @@ @article{brix_iceage_2014
 	journal = {Polish Polar Research},
 	author = {Brix, S. and Meissner, K. and Stansky, B. and Halanych, K. M. and Jennings, R. M. and Kocot, K. M. and Svavarsson, J.},
 	year = {2014},
-	note = {Publisher: -},
+	note = {Publisher: -}
+@article{meisner_benthic_2014,
+	title = {Benthic habitats around {Iceland} investigated during the {IceAGE} expeditions},
+	volume = {35},
+	issn = {0138-0338},
+	url = {http://www.scopus.com/inward/record.url?scp=84905982926&partnerID=8YFLogxK},
+	doi = {10.2478/popore-2014-0016},
+	abstract = {During the IceAGE (Icelandic marine Animals - Genetics and Ecology) expeditions in waters around Iceland and the Faroe Islands in 2011 and 2013, visual assessments of habitats and the study of surface sediment characteristics were undertaken in 119-2750 m water depth. Visual inspection was realized by means of an epibenthic sled equipped with a digital underwater video camcorder and a still camera. For determination of surface sediment characteristics a subsample of sediment from box corer samples or different grabs was collected and analyzed in the lab. Muddy bottoms predominated in the deep basins (Iceland Basin, Irminger Basin, deep Norwegian and Iceland Seas), while sand and gravel dominated on the shelves and the ridges, and in areas with high currents. Organic contents were highest in the deep Norwegian and Iceland Seas and in the Iceland Basin, and at these sites dense aggregations of mobile epibenthic organisms were observed. Large dropstones were abundant in the Iceland Sea near the shelf and in the Denmark Strait. The dropstones carried diverse, sessile epibenthic fauna, which may be underestimated using traditional sampling gear. The paper supplies new background information for studies based on IceAGE material, especially studies related to ecology and taxonomy.},
+	number = {2},
+	urldate = {2024-04-07},
+	journal = {Polish Polar Research},
+	author = {Meißner, Karin and Brenke, Nils and Svavarsson, Jörundur},
+	year = {2014},
+	keywords = {Benthic habitat, Icelandic waters, North Atlantic, Sediment characteristics, Visual assessment},
+	pages = {177--202},
+}
+@article{rogers2007corals,
+  title={Corals on seamounts},
+  author={Rogers, Alex D and Baco, Amy and Griffiths, Huw and Hart, Thomas and Hall-Spencer, Jason M},
+  journal={Seamounts: ecology, fisheries \& conservation},
+  pages={141--169},
+  year={2007},
+  publisher={Wiley Online Library}
+}
+@article{stransky_diversity_2010,
+	title = {Diversity and species composition of peracarids ({Crustacea}: {Malacostraca}) on the {South} {Greenland} shelf: spatial and temporal variation},
+	volume = {33},
+	issn = {1432-2056},
+	shorttitle = {Diversity and species composition of peracarids ({Crustacea}},
+	url = {https://doi.org/10.1007/s00300-009-0691-5},
+	doi = {10.1007/s00300-009-0691-5},
+	abstract = {The interannual variability in peracarid (Crustacea: Malacostraca; Amphipoda, Isopoda, Cumacea, Tanaidacea) species composition and diversity on the South Greenland shelf was studied at four stations over a sampling period of 3 years (2001, 2002 and 2004), using a Rauschert sled at depths of about 160 m. The South Greenland peracarids were relatively stable over the 3 years with respect to evenness and diversity. Moderate changes in temperature and salinity had negligible effects on the species composition, while sediment structure was found to be the most important environmental variable shaping the peracarid fauna.},
+	language = {en},
+	number = {2},
+	urldate = {2024-04-10},
+	journal = {Polar Biology},
+	author = {Stransky, Bente and Svavarsson, Jörundur},
+	month = feb,
+	year = {2010},
+	keywords = {Peracarida, Greenland, Shelf, Spatial and temporal variation, Species distribution},
+	pages = {125--139},
+}
+@article{havermans_genetic_2013,
+	title = {Genetic and {Morphological} {Divergences} in the {Cosmopolitan} {Deep}-{Sea} {Amphipod} {Eurythenes} gryllus {Reveal} a {Diverse} {Abyss} and a {Bipolar} {Species}},
+	volume = {8},
+	issn = {1932-6203},
+	url = {https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0074218},
+	doi = {10.1371/journal.pone.0074218},
+	abstract = {Eurythenes gryllus is one of the most widespread amphipod species, occurring in every ocean with a depth range covering the bathyal, abyssal and hadal zones. Previous studies, however, indicated the existence of several genetically and morphologically divergent lineages, questioning the assumption of its cosmopolitan and eurybathic distribution. For the first time, its genetic diversity was explored at the global scale (Arctic, Atlantic, Pacific and Southern oceans) by analyzing nuclear (28S rDNA) and mitochondrial (COI, 16S rDNA) sequence data using various species delimitation methods in a phylogeographic context. Nine putative species-level clades were identified within E. gryllus. A clear distinction was observed between samples collected at bathyal versus abyssal depths, with a genetic break occurring around 3,000 m. Two bathyal and two abyssal lineages showed a widespread distribution, while five other abyssal lineages each seemed to be restricted to a single ocean basin. The observed higher diversity in the abyss compared to the bathyal zone stands in contrast to the depth-differentiation hypothesis. Our results indicate that, despite the more uniform environment of the abyss and its presumed lack of obvious isolating barriers, abyssal populations might be more likely to show population differentiation and undergo speciation events than previously assumed. Potential factors influencing species’ origins and distributions, such as hydrostatic pressure, are discussed. In addition, morphological findings coincided with the molecular clades. Of all specimens available for examination, those of the bipolar bathyal clade seemed the most similar to the ‘true’ E. gryllus. We present the first molecular evidence for a bipolar distribution in a macro-benthic deep-sea organism.},
+	language = {en},
+	number = {9},
+	urldate = {2024-04-10},
+	journal = {PLOS ONE},
+	author = {Havermans, Charlotte and Sonet, Gontran and d’Acoz, Cédric d’Udekem and Nagy, Zoltán T. and Martin, Patrick and Brix, Saskia and Riehl, Torben and Agrawal, Shobhit and Held, Christoph},
+	month = sep,
+	year = {2013},
+	note = {Publisher: Public Library of Science},
+	keywords = {Antarctica, Cryptic speciation, Deep sea, Haplotypes, Islands, Phylogenetic analysis, Phylogeography, Population genetics},
+	pages = {e74218},
+}
+@article{wilson_historical_1998,
+	title = {Historical influences on deep-sea isopod diversity in the {Atlantic} {Ocean}},
+	volume = {45},
+	issn = {0967-0645},
+	url = {https://www.sciencedirect.com/science/article/pii/S0967064597000465},
+	doi = {10.1016/S0967-0645(97)00046-5},
+	abstract = {Most isopod crustaceans in the North Atlantic deep sea belong to the suborder Asellota. In contrast, South Atlantic isopod faunas have a significant component of flabelliferan isopods, a phylogenetic clade that contains suborders derived evolutionarily later than the Asellota. The flabelliferans decrease diversity from shallow water to deep water and on a south-to-north latitudinal gradient. Although many asellote families are endemic to the deep sea, none of the flabelliferan families appear to have evolved in the abyss. Recent colonisations of the deep sea, which may have been limited to the southern hemisphere by oceanographic conditions, have significant consequences for observed regional diversities of some taxa. Instability in oceanographic conditions owing to glaciation and benthic storms may have further limited benthic species richness of the North Atlantic deep-sea benthos.},
+	number = {1},
+	urldate = {2024-04-10},
+	journal = {Deep Sea Research Part II: Topical Studies in Oceanography},
+	author = {Wilson, George D. F.},
+	month = jan,
+	year = {1998},
+	pages = {279--301},
+}
+@article{balkenhol_identifying_2009,
+	title = {Identifying future research needs in landscape genetics: where to from here?},
+	volume = {24},
+	issn = {0921-2973},
+	journal = {Landscape Ecology},
+	author = {Balkenhol, Niko and Gugerli, Felix and Cushman, Sam A and Waits, Lisette P and Coulon, Aurélie and Arntzen, JW and Holderegger, Rolf and Wagner, Helene H and {Participants of the Landscape Genetics Research Agenda Workshop 2007}},
+	year = {2009},
+	note = {Publisher: Springer},
+	pages = {455--463},
+}
+@article{colosimo_widespread_2005,
+	title = {Widespread parallel evolution in sticklebacks by repeated fixation of ectodysplasin alleles},
+	volume = {307},
+	issn = {0036-8075},
+	number = {5717},
+	journal = {science},
+	author = {Colosimo, Pamela F and Hosemann, Kim E and Balabhadra, Sarita and Villarreal Jr, Guadalupe and Dickson, Mark and Grimwood, Jane and Schmutz, Jeremy and Myers, Richard M and Schluter, Dolph and Kingsley, David M},
+	year = {2005},
+	note = {Publisher: American Association for the Advancement of Science},
+	pages = {1928--1933},
+}
+@article{hansen_north_2000,
+	title = {North {Atlantic}–{Nordic} {Seas} exchanges},
+	volume = {45},
+	issn = {0079-6611},
+	url = {https://www.sciencedirect.com/science/article/pii/S007966119900052X},
+	doi = {10.1016/S0079-6611(99)00052-X},
+	abstract = {The northeastern part of the North Atlantic is unique in the sense that it is much warmer in the surface than other ocean areas at similar latitudes. The main reason for this is the large northward transport of heat that extends to high latitudes and crosses the Greenland–Scotland Ridge to enter the Nordic Seas and the Arctic. There the warm Atlantic water is converted to colder water masses that return southwards over the ridge partly as surface outflows and partly as overflows through the deep passages across the ridge. In this paper, the state of knowledge on the exchanges especially across the eastern part of the Greenland–Scotland Ridge is reviewed based on results from the ICES NANSEN (North Atlantic–Norwegian Sea Exchanges) project, from the Nordic WOCE project and from other sources. The accumulated evidence allows us to describe the exchanges in fair detail; the origins of the waters, the patterns of their flow towards and over the ridge and their ultimate fate. There is also increasing information on temporal variations of the exchanges although dynamical changes are still not well understood. Quantitative estimates for the volume transport of most of the overflow branches seem reasonably well established, and transport measurements of the Atlantic inflows to the Nordic Seas are approaching acceptable levels of confidence which allows preliminary budgets to be presented. The deep overflows are driven by pressure gradients set up by the formation of deep and intermediate water. The dominance of deep overflows over surface outflows in the water budget argues that this thermohaline forcing also dominates over direct wind stress and estuarine forcing in driving the Atlantic water inflow across the Greenland–Scotland Ridge, while wind stress seems to influence the characteristics and distribution of the Atlantic water north of the ridge.},
+	number = {2},
+	urldate = {2024-04-07},
+	journal = {Progress in Oceanography},
+	author = {Hansen, B and Østerhus, S},
+	month = feb,
+	year = {2000},
+	pages = {109--208},
 }
+@article{brix2010distribution,
+  title={Distribution and diversity of desmosomatid and nannoniscid isopods (Crustacea) on the Greenland--Iceland--Faeroe Ridge},
+  author={Brix, Saskia and Svavarsson, J{\"o}rundur},
+  journal={Polar Biology},
+  volume={33},
+  pages={515--530},
+  year={2010},
+  publisher={Springer}