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  • Springer  (185,425)
  • American Institute of Physics (AIP)  (29,098)
  • BioMed Central  (15,049)
  • PANGAEA  (13,624)
  • 2010-2014  (243,196)
  • 2000-2004
  • 1955-1959
  • 2013  (131,276)
  • 2011  (111,920)
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  • 2010-2014  (243,196)
  • 2000-2004
  • 1955-1959
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  • 101
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 102
    Publication Date: 2015-05-11
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 103
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 104
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 105
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 106
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 107
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 108
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 109
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 110
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 111
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 112
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 113
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 114
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    PANGAEA
    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 115
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 116
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 117
    Publication Date: 2019-07-16
    Description: In this experimental study, we compared the embryonic respiration rate in air and water of six East African sesarmid species with intertidal, supratidal and arboreal habits, to highlight possible adaptations in embryonic metabolism to their different lifestyles. The embryos of all analysed crabs showed bimodal respiration, but we did not find a trend towards an enhanced embryonic oxygen uptake in air from the intertidal to the arboreal and supratidal species. However, the late-stage embryos of the most land-adapted species, Chiromantes spp., showed an enhanced metabolism when immersed in sea water that we interpreted as an adaptive recovery mechanism to cope with the storage of by-products due to marine-based metabolic pathways during long emersion periods. Thus, we showed that the embryos of land-adapted species, although still strongly water dependent, are well adapted to semi-terrestrial habitats and represent a minor limiting factor for females, which are not restricted in their emersion period by the oxygen requirements of their embryos.
    Repository Name: EPIC Alfred Wegener Institut
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  • 118
    Publication Date: 2017-06-05
    Description: The endemic Antarctic brown macroalga Desmarestia anceps colonizes the subtidal between 5 and 30 m in Potter Cove on King George Island (South Shetland Islands, Antarctica). Experiments were conducted to study photosynthetic activities, antioxidative enzymes and UV tolerance of field-grown individuals with respect to the light histories along different subtidal positions. Individuals collected from the upper (5.5 m) and mid-subtidal (9.0 m) are characterized by high maximum electron transport rates (ETRmax) measured by PAM-fluorometry and high activities of superoxide dismutase (SOD) supported by considerable activities of glutathione reductase. Individuals of this species from the upper subtidal are able to tolerate high irradiances of UV-B radiation because its photosynthetic apparatus is putatively well protected by phlorotannins. In contrast, individuals from lower subtidal positions (13.5 and 15.5 m) showed an opposite trend: lower ETRmax and SOD activities as well as a lower UV tolerance of photosynthesis. Moreover, a non-denaturing polyacrylamide gel electrophoresis (native PAGE) of a partially purified crude extract reveals that D. anceps has probably six isoforms of SOD. These intra-specific patterns imply a high phenotypical plasticity of D. anceps with respect to its photosynthesis and photoprotective mechanisms. Overall, photosynthesis, UV tolerance and antioxidative potential are highly regulated in D. anceps corresponding to the respective light regimes along its natural growth sites.
    Repository Name: EPIC Alfred Wegener Institut
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  • 119
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Ecosystems 16 (2013): 1550-1564, doi:10.1007/s10021-013-9701-0.
    Description: We examined controls of benthic dinitrogen (N2) fixation and primary production in oligotrophic lakes in Arctic Alaska, Toolik Field Station (Arctic Long-Term Ecological Research Site). Primary production in many oligotrophic lakes is limited by nitrogen (N), and benthic processes are important for whole-lake function. Oligotrophic lakes are increasingly susceptible to low-level, non-point source nutrient inputs, yet the effects on benthic processes are not well understood. This study examines the results from a whole-lake fertilization experiment in which N and P were added at a relatively low level (4 times natural loading) in Redfield ratio to a shallow (3 m) and a deep (20 m) oligotrophic lake. The two lakes showed similar responses to fertilization: benthic primary production and respiration (each 50–150 mg C m−2 day−1) remained the same, and benthic N2 fixation declined by a factor of three- to fourfold by the second year of treatment (from ~0.35 to 0.1 mg N m−2 day−1). This showed that the response of benthic N2 fixation was de-coupled from the nutrient limitation status of benthic primary producers and raised questions about the mechanisms, which were examined in separate laboratory experiments. Bioassay experiments in intact cores also showed no response of benthic primary production to added N and P, but contrasted with the whole-lake experiment in that N2 fixation did not respond to added N, either alone or in conjunction with P. This inconsistency was likely a result of nitrogenase activity of existing N2 fixers during the relative short duration (9 days) of the bioassay experiment. N2 fixation showed a positive saturating response when light was increased in the laboratory, but was not statistically related to ambient light level in the field, leading us to conclude that light limitation of the benthos from increasing water-column production was not important. Thus, increased N availability in the sediments through direct uptake likely caused a reduction in N2 fixation. These results show the capacity of the benthos in oligotrophic systems to buffer the whole-system response to nutrient addition by the apparent ability for significant nutrient uptake and the rapid decline in N2 fixation in response to added nutrients. Reduced benthic N2 fixation may be an early indicator of a eutrophication response of lakes which precedes the transition from benthic to water-column-dominated systems.
    Description: This project was supported by NSF-OPP 9732281, NSF-DEB 9810222, NSF-DEB 0423385, and by a Doctoral Dissertation Improvement Grant NSF-DEB 0206173. Additional funding was provided by the Small Grants Program through the NSF-IGERT Program in Biogeochemistry and Environmental Change at Cornell University.
    Keywords: Benthic ; Nitrogen fixation ; Primary production ; Oligotrophic ; Arctic ; Toolik
    Repository Name: Woods Hole Open Access Server
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  • 120
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Microbiology 13 (2013): 150, doi:10.1186/1471-2180-13-150.
    Description: Deep hypersaline anoxic basins (DHABs) are isolated habitats at the bottom of the eastern Mediterranean Sea, which originate from the ancient dissolution of Messinian evaporites. The different basins have recruited their original biota from the same source, but their geological evolution eventually constituted sharp environmental barriers, restricting genetic exchange between the individual basins. Therefore, DHABs are unique model systems to assess the effect of geological events and environmental conditions on the evolution and diversification of protistan plankton. Here, we examine evidence for isolated evolution of unicellular eukaryote protistan plankton communities driven by geological separation and environmental selection. We specifically focused on ciliated protists as a major component of protistan DHAB plankton by pyrosequencing the hypervariable V4 fragment of the small subunit ribosomal RNA. Geospatial distributions and responses of marine ciliates to differential hydrochemistries suggest strong physical and chemical barriers to dispersal that influence the evolution of this plankton group. Ciliate communities in the brines of four investigated DHABs are distinctively different from ciliate communities in the interfaces (haloclines) immediately above the brines. While the interface ciliate communities from different sites are relatively similar to each other, the brine ciliate communities are significantly different between sites. We found no distance-decay relationship, and canonical correspondence analyses identified oxygen and sodium as most important hydrochemical parameters explaining the partitioning of diversity between interface and brine ciliate communities. However, none of the analyzed hydrochemical parameters explained the significant differences between brine ciliate communities in different basins. Our data indicate a frequent genetic exchange in the deep-sea water above the brines. The “isolated island character” of the different brines, that resulted from geological events and contemporary environmental conditions, create selective pressures driving evolutionary processes, and with time, lead to speciation and shape protistan community composition. We conclude that community assembly in DHABs is a mixture of isolated evolution (as evidenced by small changes in V4 primary structure in some taxa) and species sorting (as indicated by the regional absence/presence of individual taxon groups on high levels in taxonomic hierarchy).
    Description: This work was funded by NSF grants OCE-0849578 and OCE- 1061774 to VE and support from Carl Zeiss fellowship to AS and from the Deutsche Forschungsgemeinschaft (grants STO414/3-2 and STO414/7-1) to TS.
    Keywords: Ciliates ; Hypersaline ; Deep-sea anoxic basins ; DHABs ; Brine ; Species sorting ; Environmental filtering ; Niche separation
    Repository Name: Woods Hole Open Access Server
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  • 121
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeochemistry 114 (2013): 11-23, doi:10.1007/s10533-012-9801-5.
    Description: Human actions have both intentionally and unintentionally altered the global economy of nitrogen (N), with both positive and negative consequences for human health and welfare, the environment and climate change. Here we examine long-term trends in reactive N (Nr) creation and efficiencies of Nr use within the continental US. We estimate that human actions in the US have increased Nr inputs by at least ~5 times compared to pre-industrial conditions. Whereas N2 fixation as a by-product of fossil fuel combustion accounted for ~1/4 of Nr inputs from the 1970s to 2000 (or ~7 Tg N year−1), this value has dropped substantially since then (to 〈5 Tg N year−1), owing to Clean Air Act amendments. As of 2007, national N use efficiency (NUE) of all combined N inputs was equal to ~40 %. This value increases to 55 % when considering intentional N inputs alone, with food, industrial goods, fuel and fiber production accounting for the largest Nr sinks, respectively. We estimate that 66 % of the N lost during the production of goods and services enters the air (as NO x , NH3, N2O and N2), with the remaining 34 % lost to various waterways. These Nr losses contribute to smog formation, acid rain, eutrophication, biodiversity declines and climate change. Hence we argue that an improved national NUE would: (i) benefit the US economy on the production side; (ii) reduce social damage costs; and (iii) help avoid some major climate change risks in the future.
    Description: This work resulted from a workshop supported by NSF Research Coordination Network Awards DEB-0443439 and DEB-1049744 and by the David and Lucille Packard Foundation.
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  • 122
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Conservation Genetics Resources 5 (2013): 561-563, doi:10.1007/s12686-012-9852-x.
    Description: A total of one hundred microsatellites loci were selected from the draft genome of Stylophora pistillata and evaluated in previously characterized samples of Stylophora cf pistillata from the Red Sea. 17 loci were amplified successfully and tested in 24 individuals from samples belonging to a single population from the central region of the Red Sea. The number of alleles ranged from 3 to 15 alleles per locus, while observed heterozygosity ranged from 0.292 to 0.95. Six of these loci showed significant deviations from Hardy–Weinberg equilibrium (HWE) expectations, and 4/136 paired loci comparisons suggested linkage disequilibrium after Bonferroni corrections. After excluding loci with significant HWE deviation and evidence of null alleles, average genetic diversity over loci in the population studied (N = 24, Nloci = 11) was 0.701 ± 0.380. This indicates that these loci can be used effectively to evaluate genetic diversity and undertake population genetics studies in Stylophora sp. populations.
    Description: This research was funded by King Abdullah University of Science and Technology (KAUST), Saudi Arabia.
    Keywords: Stylophora ; Tetra and dinucleotide microsatellites ; Red Sea ; Coral
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  • 123
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeochemistry 115 (2013): 299-315, doi:10.1007/s10533-013-9836-2.
    Description: A series of eight watersheds on the Pacific coast of Panama where conversion of mature lowland wet forest to pastures by artisanal burning provided watershed-scale experimental units with a wide range of forest cover (23, 29, 47, 56, 66, 73, 73, 91, and 92%). We used these watersheds as a landscape-scale experiment to assess effects of degree of deforestation on within-watershed retention and hydrological export of atmospheric inputs of nutrients. Retention was estimated by comparing rainfall nutrient concentrations (volume-weighted to allow for evapotranspiration) to concentrations in freshwater reaches of receiving streams. Retention of rain-derived nutrients in these Panama watersheds averaged 77, 85, 80, and 62% for nitrate, ammonium, dissolved organic N, and phosphate, respectively. Retention of rain-derived inorganic nitrogen, however, depended on watershed cover: retention of nitrate and ammonium in pasture-dominated watersheds was 95 and 98%, while fully forested watersheds retained 65 and 80% of atmospheric nitrate and ammonium inputs. Watershed forest cover did not affect retention of dissolved organic nitrogen and phosphate. Exports from more forested watersheds yielded DIN/P near 16, while pasture-dominated watersheds exported N/P near 2. The differences in magnitude of exports and ratios suggest that deforestation in these Panamanian forests results in exports that affect growth of plants and algae in the receiving stream and estuarine ecosystems. Watershed retention of dissolved inorganic nitrogen calculated from wet plus dry atmospheric deposition varied from 90% in pasture- to 65% in forest-dominated watersheds, respectively. Discharges of DIN to receiving waters from the watersheds therefore rose from 10% of atmospheric inputs for pasture-dominated watersheds, to about 35% of atmospheric inputs for fully forested watersheds. These results from watersheds with no agriculture or urbanization, but different conversion of forest to pasture by burning, show significant, deforestation-dependent retention within tropical watersheds, but also ecologically significant, and deforestation-dependent, exports that are biologically significant because of the paucity of nutrients in receiving tropical stream and coastal waters.
    Description: This work was funded by NSF Grant BIO- 0842413
    Keywords: Tropical watersheds ; Forests ; Pastures ; Nitrogen ; Phosphorus ; Evapotranspiration ; Groundwater
    Repository Name: Woods Hole Open Access Server
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  • 124
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Evolutionary Biology 13 (2013): 187, doi:10.1186/1471-2148-13-187.
    Description: We recently reported (Curr Biol 22:683–688, 2012) that the eyes of giant and colossal squid can grow to three times the diameter of the eyes of any other animal, including large fishes and whales. As an explanation to this extreme absolute eye size, we developed a theory for visual performance in aquatic habitats, leading to the conclusion that the huge eyes of giant and colossal squid are uniquely suited for detection of sperm whales, which are important squid-predators in the depths where these squid live. A paper in this journal by Schmitz et al. (BMC Evol Biol 13:45, 2013) refutes our conclusions on the basis of two claims: (1) using allometric data they argue that the eyes of giant and colossal squid are not unexpectedly large for the size of the squid, and (2) a revision of the values used for modelling indicates that large eyes are not better for detection of approaching sperm whales than they are for any other task. We agree with Schmitz et al. that their revised values for intensity and abundance of planktonic bioluminescence may be more realistic, or at least more appropriately conservative, but argue that their conclusions are incorrect because they have not considered some of the main arguments put forward in our paper. We also present new modelling to demonstrate that our conclusions remain robust, even with the revised input values suggested by Schmitz et al.
    Keywords: Vision ; Eyes ; Giant squid ; Sperm whale ; Bioluminescence ; Mesopelagic
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  • 125
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Mobile DNA 4 (2013): 19, doi:10.1186/1759-8753-4-19.
    Description: Penelope-like elements (PLEs) are an enigmatic group of retroelements sharing a common ancestor with telomerase reverse transcriptases. In our previous studies, we identified endonuclease-deficient PLEs that are associated with telomeres in bdelloid rotifers, small freshwater invertebrates best known for their long-term asexuality and high foreign DNA content. Completion of the high-quality draft genome sequence of the bdelloid rotifer Adineta vaga provides us with the opportunity to examine its genomic transposable element (TE) content, as well as TE impact on genome function and evolution. We performed an exhaustive search of the A. vaga genome assembly, aimed at identification of canonical PLEs combining both the reverse transcriptase (RT) and the GIY-YIG endonuclease (EN) domains. We find that the RT/EN-containing Penelope families co-exist in the A. vaga genome with the EN-deficient RT-containing Athena retroelements. Canonical PLEs are present at very low copy numbers, often as a single-copy, and there is no evidence that they might preferentially co-mobilize EN-deficient PLEs. We also find that Penelope elements can participate in expansion of A. vaga multigene families via trans-action of their enzymatic machinery, as evidenced by identification of intron-containing host genes framed by the Penelope terminal repeats and characteristic target-site duplications generated upon insertion. In addition, we find that Penelope open reading frames (ORFs) in several families have incorporated long stretches of coding sequence several hundred amino acids (aa) in length that are highly enriched in asparagine residues, a phenomenon not observed in other retrotransposons. Our results show that, despite their low abundance and low transcriptional activity in the A. vaga genome, endonuclease-containing Penelope elements can participate in expansion of host multigene families. We conclude that the terminal repeats represent the cis-acting sequences required for mobilization of the intervening region in trans by the Penelope-encoded enzymatic activities. We also hypothesize that the unusual capture of long N-rich segments by the Penelope ORF occurs as a consequence of peculiarities of its replication mechanism. These findings emphasize the unconventional nature of Penelope retrotransposons, which, in contrast to all other retrotransposon types, are capable of dispersing intron-containing genes, thereby questioning the validity of traditional estimates of gene retrocopies in PLE-containing eukaryotic genomes.
    Description: This research was supported by grants MCB-0821956 and MCB-1121334 from the U.S. National Science Foundation to I.A.
    Keywords: Retrotransposon ; Reverse transcriptase ; GIY-YIG endonuclease
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  • 126
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Evolutionary Biology 12 (2012): 209, doi:10.1186/1471-2148-12-209.
    Description: Marine phytoplankton drift passively with currents, have high dispersal potentials and can be comprised of morphologically cryptic species. To examine molecular subdivision in the marine diatom Thalassiosira rotula, variations in rDNA sequence, genome size, and growth rate were examined among isolates collected from the Atlantic and Pacific Ocean basins. Analyses of rDNA included T. gravida because morphological studies have argued that T. rotula and T. gravida are conspecific. Culture collection isolates of T. gravida and T. rotula diverged by 7.0 ± 0.3% at the ITS1 and by 0.8 ± 0.03% at the 28S. Within T. rotula, field and culture collection isolates were subdivided into three lineages that diverged by 0.6 ± 0.3% at the ITS1 and 0% at the 28S. The predicted ITS1 secondary structure revealed no compensatory base pair changes among lineages. Differences in genome size were observed among isolates, but were not correlated with ITS1 lineages. Maximum acclimated growth rates of isolates revealed genotype by environment effects, but these were also not correlated with ITS1 lineages. In contrast, intra-individual variation in the multi-copy ITS1 revealed no evidence of recombination amongst lineages, and molecular clock estimates indicated that lineages diverged 0.68 Mya. The three lineages exhibited different geographic distributions and, with one exception, each field sample was dominated by a single lineage. The degree of inter- and intra-specific divergence between T. gravida and T. rotula suggests they should continue to be treated as separate species. The phylogenetic distinction of the three closely-related T. rotula lineages was unclear. On the one hand, the lineages showed no physiological differences, no consistent genome size differences and no significant changes in the ITS1 secondary structure, suggesting there are no barriers to interbreeding among lineages. In contrast, analysis of intra-individual variation in the multicopy ITS1 as well as molecular clock estimates of divergence suggest these lineages have not interbred for significant periods of time. Given the current data, these lineages should be considered a single species. Furthermore, these T. rotula lineages may be ecologically relevant, given their differential abundance over large spatial scales.
    Description: This research was supported by National Science Foundation grants, NSF 0727227 (to TAR) and NSF SBE0245039 (to URI, TAR). Part of the research was conducted using instrumentation supported by NSF-EPSCoR grants 0554548 and 1004057.
    Keywords: Phytoplankton ; Phylogeography ; Dispersal ; Physiology ; Intraspecific diversity
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  • 127
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Bioinformatics 14 (2013): 16, doi:10.1186/1471-2105-14-16.
    Description: The digitization of biodiversity data is leading to the widespread application of taxon names that are superfluous, ambiguous or incorrect, resulting in mismatched records and inflated species numbers. The ultimate consequences of misspelled names and bad taxonomy are erroneous scientific conclusions and faulty policy decisions. The lack of tools for correcting this ‘names problem’ has become a fundamental obstacle to integrating disparate data sources and advancing the progress of biodiversity science. The TNRS, or Taxonomic Name Resolution Service, is an online application for automated and user-supervised standardization of plant scientific names. The TNRS builds upon and extends existing open-source applications for name parsing and fuzzy matching. Names are standardized against multiple reference taxonomies, including the Missouri Botanical Garden's Tropicos database. Capable of processing thousands of names in a single operation, the TNRS parses and corrects misspelled names and authorities, standardizes variant spellings, and converts nomenclatural synonyms to accepted names. Family names can be included to increase match accuracy and resolve many types of homonyms. Partial matching of higher taxa combined with extraction of annotations, accession numbers and morphospecies allows the TNRS to standardize taxonomy across a broad range of active and legacy datasets. We show how the TNRS can resolve many forms of taxonomic semantic heterogeneity, correct spelling errors and eliminate spurious names. As a result, the TNRS can aid the integration of disparate biological datasets. Although the TNRS was developed to aid in standardizing plant names, its underlying algorithms and design can be extended to all organisms and nomenclatural codes. The TNRS is accessible via a web interface at http://tnrs.iplantcollaborative.org/ webcite and as a RESTful web service and application programming interface. Source code is available at https://github.com/iPlantCollaborativeOpenSource/TNRS/ webcite.
    Description: BJE was supported by NSF grant DBI 0850373 and TR by CSIRO Marine and Atmospheric Research, Australia,. BB and BJE acknowledge early financial support from Conservation International and TEAM who funded the development of early prototypes of taxonomic name resolution. The iPlant Collaborative (http://www.iplantcollaborative.org) is funded by a grant from the National Science Foundation (#DBI-0735191).
    Keywords: Biodiversity informatics ; Database integration ; Taxonomy ; Plants
    Repository Name: Woods Hole Open Access Server
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  • 128
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Mobile DNA 3 (2012): 19, doi:10.1186/1759-8753-3-19.
    Description: The third international conference on the genomic impact of eukaryotic transposable elements (TEs) was held 24 to 28 February 2012 at the Asilomar Conference Center, Pacific Grove, CA, USA. Sponsored in part by the National Institutes of Health grant 5 P41 LM006252, the goal of the conference was to bring together researchers from around the world who study the impact and mechanisms of TEs using multiple computational and experimental approaches. The meeting drew close to 170 attendees and included invited floor presentations on the biology of TEs and their genomic impact, as well as numerous talks contributed by young scientists. The workshop talks were devoted to computational analysis of TEs with additional time for discussion of unresolved issues. Also, there was ample opportunity for poster presentations and informal evening discussions. The success of the meeting reflects the important role of Repbase in comparative genomic studies, and emphasizes the need for close interactions between experimental and computational biologists in the years to come.
    Description: The conference was supported in part by the National Institutes of Health grant 5 P41 LM006252.
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  • 129
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in EvoDevo 4 (2013): 16, doi:10.1186/2041-9139-4-16.
    Description: The de novo assembly of transcriptomes from short shotgun sequences raises challenges due to random and non-random sequencing biases and inherent transcript complexity. We sought to define a pipeline for de novo transcriptome assembly to aid researchers working with emerging model systems where well annotated genome assemblies are not available as a reference. To detail this experimental and computational method, we used early embryos of the sea anemone, Nematostella vectensis, an emerging model system for studies of animal body plan evolution. We performed RNA-seq on embryos up to 24 h of development using Illumina HiSeq technology and evaluated independent de novo assembly methods. The resulting reads were assembled using either the Trinity assembler on all quality controlled reads or both the Velvet and Oases assemblers on reads passing a stringent digital normalization filter. A control set of mRNA standards from the National Institute of Standards and Technology (NIST) was included in our experimental pipeline to invest our transcriptome with quantitative information on absolute transcript levels and to provide additional quality control. We generated 〉200 million paired-end reads from directional cDNA libraries representing well over 20 Gb of sequence. The Trinity assembler pipeline, including preliminary quality control steps, resulted in more than 86% of reads aligning with the reference transcriptome thus generated. Nevertheless, digital normalization combined with assembly by Velvet and Oases required far less computing power and decreased processing time while still mapping 82% of reads. We have made the raw sequencing reads and assembled transcriptome publically available. Nematostella vectensis was chosen for its strategic position in the tree of life for studies into the origins of the animal body plan, however, the challenge of reference-free transcriptome assembly is relevant to all systems for which well annotated gene models and independently verified genome assembly may not be available. To navigate this new territory, we have constructed a pipeline for library preparation and computational analysis for de novo transcriptome assembly. The gene models defined by this reference transcriptome define the set of genes transcribed in early Nematostella development and will provide a valuable dataset for further gene regulatory network investigations.
    Keywords: Transcriptome ; Gene regulatory network ; Nematostella embryonic development ; Body plan evolution ; Next-generation sequencing ; Illumina HiSeq ; Trinity ; Oases ; RNA-seq
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  • 130
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Reviews in Fish Biology and Fisheries 23 (2013): 317-364, doi:10.1007/s11160-012-9297-z.
    Description: A recent survey lists more than 100 papers utilizing the auditory evoked potential (AEP) recording technique for studying hearing in fishes. More than 95 % of these AEP-studies were published after Kenyon et al. introduced a non-invasive electrophysiological approach in 1998 allowing rapid evaluation of hearing and repeated testing of animals. First, our review compares AEP hearing thresholds to behaviorally gained thresholds. Second, baseline hearing abilities are described and compared in 111 fish species out of 51 families. Following this, studies investigating the functional significance of various accessory hearing structures (Weberian ossicles, swim bladder, otic bladders) by eliminating these morphological structures in various ways are dealt with. Furthermore, studies on the ontogenetic development of hearing are summarized. The AEP-technique was frequently used to study the effects of high sound/noise levels on hearing in particular by measuring the temporary threshold shifts after exposure to various noise types (white noise, pure tones and anthropogenic noises). In addition, the hearing thresholds were determined in the presence of noise (white, ambient, ship noise) in several studies, a phenomenon termed masking. Various ecological (e.g., temperature, cave dwelling), genetic (e.g., albinism), methodical (e.g., ototoxic drugs, threshold criteria, speaker choice) and behavioral (e.g., dominance, reproductive status) factors potentially influencing hearing were investigated. Finally, the technique was successfully utilized to study acoustic communication by comparing hearing curves with sound spectra either under quiet conditions or in the presence of noise, by analyzing the temporal resolution ability of the auditory system and the detection of temporal, spectral and amplitude characteristics of conspecific vocalizations.
    Description: Support from the Austrian Science Fund (FWF grant 22319 to F.L.).
    Keywords: AEP ; Hearing ; Sound pressure level ; Particle acceleration levels ; Thresholds ; Noise ; Ontogeny ; Communication
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  • 131
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Marine Biodiversity 43 (2013): 237-241, doi:10.1007/s12526-013-0151-x.
    Description: Despite the ubiquitous role sponges play in reef ecosystem dynamics, little is known about population-level connectivity in these organisms. The general field of population genetics in sponges remains in its infancy. To date, microsatellite markers have only been developed for few sponge species and no sponge population genetics studies using microsatellites have been conducted in the Red Sea. Here, with the use of next-generation sequencing, we characterize 12 novel polymorphic loci for the common reef sponge, Stylissa carteri. The number of alleles per loci ranged between three and eight. Observed heterozygosity frequencies (Ho) ranged from 0.125 to 0.870, whereas expected (He) heterozygosity frequencies ranged from 0.119 to 0.812. Only one locus showed consistent deviations from Hardy-Weinberg equilibrium (HWE) in both populations and two loci consistently showed the possible presence of null alleles. No significant linkage disequilibrium was detected for any pairs of loci. These microsatellites will be of use for numerous ecological studies focused on this common and abundant sponge.
    Description: This work was funded by the King Abdullah University of Science and Technology.
    Keywords: Microsatellites ; Sponges ; Population genetics ; Connectivity ; Stylissa carteri
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    Publication Date: 2019-07-17
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    Publication Date: 2019-07-17
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    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
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    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
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    In:  EPIC3Bremerhaven, PANGAEA
    Publication Date: 2018-08-10
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  • 138
    Publication Date: 2019-07-17
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  • 139
    Publication Date: 2022-03-25
    Description: Polygon tundra characterizes large areas of arctic lowlands. The micro-relief pattern within polygons offers differentiated habitats for testate amoeba (testacean)communities. The objective of this study was to relate testacean species distribution within a polygon to the environmental setting. Therefore, testaceans from four cryosol pits dug at different locations within a low-centered polygon were studied in the context of pedological and pedochemical data, while ground temperature and ground moisture were measured over one summer season. The study site is located on the Berelekh River floodplain (Indigirka lowland, East Siberia). The environmental data sets reflect variations along the rim-to-center transect of the polygon and in different horizons of each pit. The testacean species distribution is mainly controlled by the soil moisture regime and pH. Most of the identified testaceans are cosmopolitans; eight species are described from an arctic environment for the first time. Differences in environmental conditions are controlled by the micro-relief of polygon tundra and must be considered in arctic lowland testacean research because they bias species composition and any further (paleo-)ecological interpretation.
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  • 140
    Publication Date: 2022-05-26
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Genomics 14 (2013): 412, doi:10.1186/1471-2164-14-412.
    Description: Sexual reproduction is a widely studied biological process because it is critically important to the genetics, evolution, and ecology of eukaryotes. Despite decades of study on this topic, no comprehensive explanation has been accepted that explains the evolutionary forces underlying its prevalence and persistence in nature. Monogonont rotifers offer a useful system for experimental studies relating to the evolution of sexual reproduction due to their rapid reproductive rate and close relationship to the putatively ancient asexual bdelloid rotifers. However, little is known about the molecular underpinnings of sex in any rotifer species. We generated mRNA-seq libraries for obligate parthenogenetic (OP) and cyclical parthenogenetic (CP) strains of the monogonont rotifer, Brachionus calyciflorus, to identify genes specific to both modes of reproduction. Our differential expression analysis identified receptors with putative roles in signaling pathways responsible for the transition from asexual to sexual reproduction. Differential expression of a specific copy of the duplicated cell cycle regulatory gene CDC20 and specific copies of histone H2A suggest that such duplications may underlie the phenotypic plasticity required for reproductive mode switch in monogononts. We further identified differential expression of genes involved in the formation of resting eggs, a process linked exclusively to sex in this species. Finally, we identified transcripts from the bdelloid rotifer Adineta ricciae that have significant sequence similarity to genes with higher expression in CP strains of B. calyciflorus. Our analysis of global gene expression differences between facultatively sexual and exclusively asexual populations of B. calyciflorus provides insights into the molecular nature of sexual reproduction in rotifers. Furthermore, our results offer insight into the evolution of obligate asexuality in bdelloid rotifers and provide indicators important for the use of monogononts as a model system for investigating the evolution of sexual reproduction.
    Description: This work was funded by National Institutes of Health Institute of General Medical Sciences (grant number 5R01GM079484, to JML and DMW).
    Keywords: Evolution of sexual reproduction ; Differential expression analysis ; Gene ontology analysis ; Meiosis ; Gametogenesis ; Resting eggs ; Mixis induction
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  • 141
    Publication Date: 2022-05-26
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Genomics 14 (2013): 266, doi:10.1186/1471-2164-14-266.
    Description: Nematostella vectensis, a burrowing sea anemone, has become a popular species for the study of cnidarian development. In previous studies, the expression of a variety of genes has been characterized during N. vectensis development with in situ mRNA hybridization. This has provided detailed spatial resolution and a qualitative perspective on changes in expression. However, little is known about broad transcriptome-level patterns of gene expression through time. Here we examine the expression of N. vectensis genes through the course of development with quantitative RNA-seq. We provide an overview of changes in the transcriptome through development, and examine the maternal to zygotic transition, which has been difficult to investigate with other tools. We measured transcript abundance in N. vectensis with RNA-seq at six time points in development: zygote (2 hours post fertilization (HPF)), early blastula (7 HPF), mid-blastula (12 HPF), gastrula (24 HPF), planula (5 days post fertilization (DPF)) and young polyp (10 DPF). The major wave of zygotic expression appears between 7–12 HPF, though some changes occur between 2–7 HPF. The most dynamic changes in transcript abundance occur between the late blastula and early gastrula stages. More transcripts are upregulated between the gastrula and planula than downregulated, and a comparatively lower number of transcripts significantly change between planula and polyp. Within the maternal to zygotic transition, we identified a subset of maternal factors that decrease early in development, and likely play a role in suppressing zygotic gene expression. Among the first genes to be expressed zygotically are genes whose proteins may be involved in the degradation of maternal RNA. The approach presented here is highly complementary to prior studies on spatial patterns of gene expression, as it provides a quantitative perspective on a broad set of genes through time but lacks spatial resolution. In addition to addressing the problems identified above, our work provides an annotated matrix that other investigators can use to examine genes and developmental events that we do not examine in detail here.
    Description: This work was supported by seed funds from the Brown-MBL Partnership and the National Science Foundation Graduate Student Research Fellowship. Infrastructure for data transfer from the sequencer was supported by the National Science Foundation EPSCoR Program under Grant No. 1004057 (Infrastructure to Advance Life Sciences in the Ocean State).
    Keywords: Nematostella vectensis ; Transcriptome ; Gene expression ; Maternal to zygotic transition ; Development
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  • 142
    Publication Date: 2022-05-26
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Marine Biology 160 (2013): 1773-1787, doi:10.1007/s00227-012-2031-5.
    Description: Ocean acidification is increasingly recognized as a component of global change that could have a wide range of impacts on marine organisms, the ecosystems they live in, and the goods and services they provide humankind. Assessment of these potential socio-economic impacts requires integrated efforts between biologists, chemists, oceanographers, economists and social scientists. But because ocean acidification is a new research area, significant knowledge gaps are preventing economists from estimating its welfare impacts. For instance, economic data on the impact of ocean acidification on significant markets such as fisheries, aquaculture and tourism are very limited (if not non-existent), and non-market valuation studies on this topic are not yet available. Our paper summarizes the current understanding of future OA impacts and sets out what further information is required for economists to assess socio-economic impacts of ocean acidification. Our aim is to provide clear directions for multidisciplinary collaborative research.
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  • 143
    Publication Date: 2022-05-26
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Bioinformatics 13 (2012): 211, doi:10.1186/1471-2105-13-211.
    Description: A scientific name for an organism can be associated with almost all biological data. Name identification is an important step in many text mining tasks aiming to extract useful information from biological, biomedical and biodiversity text sources. A scientific name acts as an important metadata element to link biological information. We present NetiNeti (Name Extraction from Textual Information-Name Extraction for Taxonomic Indexing), a machine learning based approach for recognition of scientific names including the discovery of new species names from text that will also handle misspellings, OCR errors and other variations in names. The system generates candidate names using rules for scientific names and applies probabilistic machine learning methods to classify names based on structural features of candidate names and features derived from their contexts. NetiNeti can also disambiguate scientific names from other names using the contextual information. We evaluated NetiNeti on legacy biodiversity texts and biomedical literature (MEDLINE). NetiNeti performs better (precision = 98.9% and recall = 70.5%) compared to a popular dictionary based approach (precision = 97.5% and recall = 54.3%) on a 600-page biodiversity book that was manually marked by an annotator. On a small set of PubMed Central’s full text articles annotated with scientific names, the precision and recall values are 98.5% and 96.2% respectively. NetiNeti found more than 190,000 unique binomial and trinomial names in more than 1,880,000 PubMed records when used on the full MEDLINE database. NetiNeti also successfully identifies almost all of the new species names mentioned within web pages. We present NetiNeti, a machine learning based approach for identification and discovery of scientific names. The system implementing the approach can be accessed at http://namefinding.ubio.org.
    Description: This project was funded by the Ellison Medical Foundation and a grant from the National Library of Medicine (R01 LM009725).
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  • 144
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    In:  EPIC3Earth System Science: Bridging the gaps between disciplines—A multi-disciplinary Helmholtz Graduate Research School, Berlin Heidelberg, Springer, 7 p., pp. 83-89, ISBN: 978-3-642-32235-8
    Publication Date: 2023-06-21
    Description: Geophysical data acquired along the Antarctic passive margins constrain the structure and geometry of the deformed continental crust. Crustal thickness estimates range between 7 and 50 km and the Antarctic continent–ocean transition zone (COTZ) extends up to 100–670 km towards the ocean. Continental deformation prior to rifting over a c. 100 million years long time span resulted in crustal stretching factors varying between 1.8 and 5.9. The time span of deformation was sufficiently large and the rifting velocity low enough to extend the margin by up to 300–400 km. Crustal thinning generates a significant subsidence and shallow water passages might already have developed during the rifting phase along the margin. Accounting for accurate continental margin deformation has also consequences for plate-tectonic reconstructions.
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  • 145
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    In:  EPIC3Earth System Science: Bridging the Gaps between Disciplines Perspectives from a Multi-disciplinary Helmholtz Research School, Heidelbert, Springer, 138 p., pp. 1-8, ISBN: 978-3-642-32234-1
    Publication Date: 2023-06-21
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  • 146
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    In:  EPIC3Earth System Science: Bridging the Gaps between Disciplines Perspectives from a Multi-disciplinary Helmholtz Research School, Heidelberg, Springer, 138 p., pp. 1-3, ISBN: 978-3-642-32234-1
    Publication Date: 2023-06-21
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    In:  EPIC3Earth System Modelling - Volume 6: ESM Data Archives in the Times of the Grid, Springer Briefs in Earth System Sciences, Berlin, Heidelberg, Springer, pp. 49-60, ISBN: 978-3-642-37243-8
    Publication Date: 2023-06-21
    Description: Grid technology can help scientists to overcome problems with the Data Deluge in climate research, as it facilitates large scale data sharing and reuse of data. Worldwide there are different initiatives to facilitate data handling for scientific work and to built up collaborational working environments with interinstitutional data access.
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  • 148
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    In:  EPIC3Earth System Science: Bridging the Gaps between Disciplines. Perspectives from a Multi-disciplinary Helmholtz Graduate Research School, Earth System Science: Bridging the Gaps between Disciplines. Perspectives from a Multi-disciplinary Helmholtz Graduate Research School, Heidleberg, Springer, 4 p., pp. 38-41, ISBN: 978-3-642-32234-1
    Publication Date: 2023-06-21
    Description: Growth of phytoplankton in the Southern Ocean (SO) is largely limited by insufficient concentrations of the micronutrient iron, so that despite the large macronutrient reservoir, the SO is considered a High Nutrient Low Chlorophyll region. Therefore, phytoplankton growth is enhanced where exogenous iron is introduced to the system, for example downstream from islands. These confined regions sustain very rich ecosystems and are hot spots for atmospheric carbon dioxide drawdown. In this study, a combination of satellite derived measurements and model simulations are used to investigate the biological and physical environmental disturbances of the island of South Georgia (37°W, 54°S), which is located in the southwestern part of the Atlantic sector of the SO. We show not only that the island shelf is an important source of dissolved iron to the system, but also that the characteristic surface circulation patterns found downstream of the island play an important role in maintaining the shape and distribution of the developing phytoplankton bloom.
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  • 149
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    In:  EPIC3Earth system science: bridging the gap between disciplines, Earth system science: bridging the gap between disciplines, Heidelberg, Springer, 7 p., pp. 97-103, ISBN: 978-3-642-32234-1
    Publication Date: 2023-06-21
    Description: Information about past environmental conditions is preserved in the elemental signature of biogenic marine carbonates. Thus, trace element to calcium ratios (Me/Ca) of biogenic calcium carbonates, such as bivalve shells, are often used to reconstruct past environmental conditions at the time of carbonate formation (Foster et al., 2008). In this study, we examine the suitability of the long-lived (〉 400 years) bivalve Arctica islandica as a high-resolution bioarchive by measuring Me/Ca ratios in the shell carbonate. Pb/Ca concentrations in A. islandica shells reflect anthropogenic gasoline lead consumption and further provide a centennial record of lead pollution for the collection site off the coast of Virginia, USA. With A. islandica shells from the North Sea we test the hypothesis that Ba/Ca and Mn/Ca ratios are indicators of the diatom abundance. Our results indicate that statistically both ratios correlate well with the diatom abundance, and yet, on a year-to-year base, there is no consistent reflection of diatom abundance patterns in the Ba/Ca and Mn/Ca annual profiles. These findings indicate that primary production affects Ba/Ca and Mn/Ca shell ratios, though we suggest that both elements are coupled to primary production through different processes and are affected by further, yet unknown processes.
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    In:  Springer atmospheric sciences
    Publication Date: 2020-02-12
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  • 151
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    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
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  • 152
    Publication Date: 2022-11-29
    Description: Living microorganisms inhabit every environment of the biosphere but only in the last decades their importance governing biochemical cycles in deep sediments has been widely recognized. Most investigations have been accomplished in the marine realm whereas there is a clear paucity of comparable studies in lacustrine sediments. One of the main challenges is to define geomicrobiological proxies that can be used to identify different microbial signals in the sediments. Laguna Potrok Aike, a maar lake located in Southeastern Patagonia, has an annually not stratifying cold water column with temperatures ranging between 4 and 10 °C, and most probably an anoxic water/sediment interface. These unusual features make it a peculiar and interesting site for geomicrobiological studies. Living microbial activity within the sediments was inspected by the first time in a sedimentary core retrieved during an ICDP-sponsored drilling operation. The main goals to study this cold subsaline environment were to characterize the living microbial consortium; to detect early diagenetic signals triggered by active microbes; and to investigate plausible links between climate and microbial populations. Results from a meter long gravity core suggest that microbial activity in lacustrine sediments can be sustained deeper than previously thought due to their adaptation to both changing temperature and oxygen availability. A multi-proxy study of the same core allowed defining past water column conditions and further microbial reworking of the organic fraction within the sediments. Methane content shows a gradual increase with depth as a result of the fermentation of methylated substrates, first methanogenic pathway to take place in the shallow subsurface of freshwater and subsaline environments. Statistical analyses of DGGE microbial diversity profiles indicate four clusters for Bacteria reflecting layered communities linked to the oxidant type whereas three clusters characterize Archaea communities that can be linked to both denitrifiers and methanogens. Independent sedimentary and biological proxies suggest that organic matter production and/or preservation have been lower during the Medieval Climate Anomaly (MCA) coinciding with a low microbial colonization of the sediments. Conversely, a reversed trend with higher organic matter content and substantial microbial activity characterizes the sediments deposited during the Little Ice Age (LIA). Thus, the initial sediments deposited during distinctive time intervals under contrasting environmental conditions have to be taken into account to understand their impact on the development of microbial communities throughout the sediments and their further imprint on early diagenetic signals.
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  • 153
    Publication Date: 2022-11-29
    Description: Authigenic minerals can form in the water column and sediments of lakes, either abiotically or mediated by biological activity. Such minerals have been used as paleosalinity and paleoproductivity indicators and reflect trophic state and early diagenetic conditions. They are also considered potential indicators of past and perhaps ongoing microbial activity within sediments. Authigenic concretions, including vivianite, were described in late glacial sediments of Laguna Potrok Aike, a maar lake in southernmost Argentina. Occurrence of iron phosphate implies specific phosphorus sorption behavior and a reducing environment, with methane present. Because organic matter content in these sediments was generally low during glacial times, there must have been alternative sources of phosphorus and biogenic methane. Identifying these sources can help define past trophic state of the lake and diagenetic processes in the sediments. We used scanning electron microscopy, phosphorus speciation in bulk sediment, pore water analyses, in situ ATP measurements, microbial cell counts, and measurements of methane content and its carbon isotope composition (d13C CH4) to identify components of and processes in the sediment. The multiple approaches indicated that volcanic materials in the catchment are important suppliers of iron, sulfur and phosphorus. These elements influence primary productivity and play a role in microbial metabolism during early diagenesis. Authigenic processes led to the formation of pyrite framboids and revealed sulfate reduction. Anaerobic oxidation of methane and shifts in pore water ion concentration indicated microbial influence with depth. This study documents the presence of active microbes within the sediments and their relationship to changing environmental conditions. It also illustrates the substantial role played by microbes in the formation of Laguna Potrok Aike concretions. Thus, authigenic minerals can be used as biosignatures in these late Pleistocene maar sediments.
    Type: info:eu-repo/semantics/workingPaper
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  • 154
    facet.materialart.
    Unknown
    Springer
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/book
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  • 155
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Möller, Lars; Sowers, Todd A; Bock, Michael; Spahni, Renato; Behrens, Melanie; Schmitt, Jochen; Miller, Heinz; Fischer, Hubertus (2013): Independent variations of CH4 emissions and isotopic composition over the past 160,000 years. Nature Geoscience, 6, 885-890, https://doi.org/10.1038/ngeo1922
    Publication Date: 2023-03-16
    Description: The response of natural CH4 sources to climate changes will be an important factor to consider as concentrations of this potent greenhouse gas continue to increase. Polar ice cores provide the means to assess this sensitivity in the past and have shown a close connection between CH4 levels and northern hemisphere temperature variability over the last glacial cycle. However, the contribution of the various CH4 sources and sinks to these changes is still a matter of debate. Contemporaneous stable CH4 isotope records in ice cores provide additional boundary conditions for assessing changes in the CH4 sources and sinks. Here we present new ice core CH4 isotope data covering the last 160,000 years, showing a clear decoupling between CH4 loading and carbon isotopic variations over most of the record. We suggest that d13CH4 variations were not dominated by a change in the source mix but rather by climate- and CO2-related ecosystem control on the isotopic composition of the methane precursor material, especially in seasonally inundated wetlands in the tropics. In contrast, relatively stable d13CH4 intervals occurred during large CH4 loading changes concurrently with past climate changes implying that most CH4 sources (most notably tropical wetlands) responded simultaneously.
    Keywords: EPICA; European Project for Ice Coring in Antarctica
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 156
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; Corumba_reservoir; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 3620 data points
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  • 157
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Estreito_reservoir; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 2579 data points
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  • 158
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itumbiara; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 29501 data points
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  • 159
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; Serra_da_Mesa_reservoir; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 1708 data points
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  • 160
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Estreito_reservoir; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 20847 data points
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  • 161
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Funil_reservoir; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 53707 data points
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  • 162
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit); Xingo_reservoir
    Type: Dataset
    Format: text/tab-separated-values, 4292 data points
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  • 163
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; G. O. Sars (2003); GS13/101; GS13/101_01; GS13/101_02; GS13/101_03; GS13/101_04; GS13/101_05; GS13/101_06; GS13/101_07; GS13/101_08; GS13/101_09; GS13/101_10; GS13/101_11; GS13/101_12; GS13/101_13; GS13/101_14; GS13/101_15; GS13/101_16; GS13/101_17; GS13/101_18; GS13/101_19; GS13/101_20; GS13/101_21; GS13/101_22; GS13/101_23; GS13/101_24; GS13/101_25; GS13/101_26; GS13/101_27; GS13/101_28; GS13/101_29; GS13/101_30; GS13/101_31; GS13/101_32; GS13/101_33; GS13/101_34; GS13/101_35; GS13/101_36; GS13/101_37; GS13/101_38; GS13/101_39; GS13/101_40; GS13/101_41; GS13/101_42; GS13/101_43; GS13/101_44; GS13/101_45; GS13/101_46; GS13/101_47; GS13/101_48; GS13/101_49; GS13/101_50; GS13/101_51; GS13/101_52; GS13/101_53; GS13/101_54; GS13/101_55; GS13/101_56; GS13/101_57; GS13/101_58; GS13/101_59; GS13/101_60; GS13/101_61; GS13/101_62; GS13/101_63; GS13/101_64; GS13/101_65; GS13/101_66; GS13/101_67; GS13/101_68; GS13/101_69; GS13/101_70; GS13/101_71; GS13/101_72; GS13/101_73; GS13/101_74; GS13/101_75; GS13/101_76; GS13/101_77; GS13/101_78; GS13/101_79; GS13/101_80; GS13/101_81; GS13/101_82; GS13/101_83; GS13/101_84; GS13/101_85; GS13/101_86; GS13/101_87; GS13/101_88; GS13/101_89; GS13/101_90; GS13/101_91; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Norwegian Sea; Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 37395 data points
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  • 164
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; Nitrate; North Sea; Norwegian Sea; Phosphate; Pressure, water; Salinity; Scotia; Scotia13/2; Scotia13/2_01; Scotia13/2_02; Scotia13/2_03; Scotia13/2_04; Scotia13/2_05; Scotia13/2_06; Scotia13/2_07; Scotia13/2_08; Scotia13/2_09; Scotia13/2_10; Scotia13/2_11; Scotia13/2_12; Scotia13/2_13; Scotia13/2_14; Scotia13/2_15; Scotia13/2_16; Scotia13/2_17; Scotia13/2_18; Scotia13/2_19; Scotia13/2_20; Scotia13/2_21; Scotia13/2_22; Scotia13/2_23; Scotia13/2_24; Scotia13/2_25; Scotia13/2_26; Scotia13/2_27; Scotia13/2_28; Scotia13/2_29; Scotia13/2_30; Scotia13/2_31; Scotia13/2_32; Scotia13/2_33; Scotia13/2_34; Scotia13/2_35; Scotia13/2_36; Scotia13/2_37; Scotia13/2_38; Scotia13/2_39; Scotia13/2_40; Scotia13/2_41; Scotia13/2_42; Scotia13/2_43; Scotia13/2_44; Scotia13/2_45; Scotia13/2_46; Scotia13/2_47; Scotia13/2_48; Scotia13/2_49; Scotia13/2_50; Scotia13/2_51; Scotia13/2_52; Scotia13/2_53; Scotia13/2_54; Scotia13/2_55; Scotia13/2_56; Silicate; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 16845 data points
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  • 165
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Dana01/13; Dana13_001; Dana13_003; Dana13_005; Dana13_008; Dana13_017; Dana13_019; Dana13_021; Dana13_025; Dana13_026; Dana13_034; Dana13_037; Dana13_039; Dana13_041; Dana13_043; Dana13_053; Dana13_056; Dana13_058; Dana13_064; Dana13_067; Dana13_068; Dana13_071; Dana13_079; Dana13_081; Dana13_084; Dana13_092; Dana13_102; Dana13_104; Dana13_106; Dana13_109; Dana13_116; Dana13_118; Dana13_120; Dana13_123; Dana13_129; Dana13_131; Dana13_133; Dana13_136; Dana13_142; Dana13_144; Dana13_146; Dana13_149; Dana13_150; Dana13_152; Dana13_154; Dana13_157; Dana II; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Kattegat; Latitude of event; Longitude of event; Pressure, water; Salinity; Skagerrak; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1222 data points
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  • 166
    facet.materialart.
    Unknown
    PANGAEA
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; English Channel; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Oxygen; Pressure, water; Salinity; Temperature, water; Thalassa; Thalassa13/1; Thalassa13/1_001; Thalassa13/1_003; Thalassa13/1_006; Thalassa13/1_007; Thalassa13/1_008; Thalassa13/1_009; Thalassa13/1_010; Thalassa13/1_011; Thalassa13/1_012; Thalassa13/1_013; Thalassa13/1_014; Thalassa13/1_015; Thalassa13/1_016; Thalassa13/1_017; Thalassa13/1_018; Thalassa13/1_019; Thalassa13/1_020; Thalassa13/1_021; Thalassa13/1_022; Thalassa13/1_023; Thalassa13/1_024; Thalassa13/1_025; Thalassa13/1_026; Thalassa13/1_027; Thalassa13/1_029; Thalassa13/1_030; Thalassa13/1_031; Thalassa13/1_032; Thalassa13/1_033; Thalassa13/1_034; Thalassa13/1_035; Thalassa13/1_036; Thalassa13/1_037; Thalassa13/1_038; Thalassa13/1_039; Thalassa13/1_040; Thalassa13/1_041; Thalassa13/1_042; Thalassa13/1_043; Thalassa13/1_044; Thalassa13/1_045; Thalassa13/1_046; Thalassa13/1_047; Thalassa13/1_048; Thalassa13/1_049; Thalassa13/1_050; Thalassa13/1_051; Thalassa13/1_052; Thalassa13/1_053; Thalassa13/1_054; Thalassa13/1_055; Thalassa13/1_056; Thalassa13/1_057; Thalassa13/1_058; Thalassa13/1_059; Thalassa13/1_060; Thalassa13/1_061; Thalassa13/1_062; Thalassa13/1_063; Thalassa13/1_063b; Thalassa13/1_064; Thalassa13/1_065; Thalassa13/1_066; Thalassa13/1_067; Thalassa13/1_068; Thalassa13/1_069; Thalassa13/1_070; Thalassa13/1_071; Thalassa13/1_072; Thalassa13/1_073; Thalassa13/1_074; Thalassa13/1_075; Thalassa13/1_076; Thalassa13/1_077; Thalassa13/1_078; Thalassa13/1_079; Thalassa13/1_080; Thalassa13/1_081; Thalassa13/1_082; Thalassa13/1_083; Thalassa13/1_084; Thalassa13/1_085; Thalassa13/1_086; Thalassa13/1_087; Thalassa13/1_089; Thalassa13/1_090; Thalassa13/1_091; Thalassa13/1_092; Thalassa13/1_093; Thalassa13/1_094; Thalassa13/1_095; Thalassa13/1_096; Thalassa13/1_097; Thalassa13/1_098; Thalassa13/1_099; Thalassa13/1_100; Thalassa13/1_101; Thalassa13/1_102; Thalassa13/1_103; Thalassa13/1_104; Thalassa13/1_105; Thalassa13/1_106; Thalassa13/1_107; Thalassa13/1_108; Thalassa13/1_109; Thalassa13/1_110; Thalassa13/1_111; Thalassa13/1_112; Thalassa13/1_113; Thalassa13/1_114; Thalassa13/1_115; Thalassa13/1_116; Thalassa13/1_117; Thalassa13/1_118; Thalassa13/1_119; Thalassa13/1_120; Thalassa13/1_121; Thalassa13/1_122; Thalassa13/1_123; Thalassa13/1_124; Thalassa13/1_125; Thalassa13/1_126; Thalassa13/1_127; Thalassa13/1_128; Thalassa13/1_129; Thalassa13/1_130; Thalassa13/1_131; Thalassa13/1_132; Thalassa13/1_133; Thalassa13/1_134; Thalassa13/1_135; Thalassa13/1_136; Thalassa13/1_137; Thalassa13/1_138; Thalassa13/1_139; Thalassa13/1_140; Thalassa13/1_141; Thalassa13/1_142; Thalassa13/1_143; Thalassa13/1_144; Thalassa13/1_145; Thalassa13/1_146; Thalassa13/1_147; Thalassa13/1_148; Thalassa13/1_149; Thalassa13/1_150; Thalassa13/1_151; Thalassa13/1_152; Thalassa13/1_153; Thalassa13/1_154; Thalassa13/1_155; Thalassa13/1_156; Thalassa13/1_157; Thalassa13/1_158; Thalassa13/1_159; Thalassa13/1_160; Thalassa13/1_161; Thalassa13/1_162; Thalassa13/1_163; Thalassa13/1_164; Thalassa13/1_165; Thalassa13/1_166; Thalassa13/1_167; Thalassa13/1_168; Thalassa13/1_169
    Type: Dataset
    Format: text/tab-separated-values, 5545 data points
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  • 167
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Pressure, water; Salinity; Temperature, water; Walther Herwig III; WH362; WH362_097; WH362_098; WH362_099; WH362_100; WH362_110; WH362_111; WH362_112; WH362_113; WH362_123; WH362_124; WH362_125; WH362_126; WH362_127; WH362_128; WH362_129; WH362_135; WH362_138; WH362_139; WH362_148; WH362_149; WH362_150; WH362_151; WH362_158; WH362_159; WH362_160; WH362_161; WH362_167; WH362_168; WH362_169; WH362_170; WH362_179; WH362_180; WH362_181; WH362_182; WH362_191; WH362_192; WH362_193; WH362_194; WH362_201; WH362_202; WH362_203; WH362_204; WH362_212; WH362_213; WH362_214; WH362_223; WH362_224; WH362_225; WH362_234; WH362_239; WH362_240; WH362_241; WH362_242; WH362_251; WH362_252; WH362_253; WH362_254; WH362_262; WH362_263; WH362_272; WH362_273; WH362_274; WH362_279; WH362_280; WH362_281
    Type: Dataset
    Format: text/tab-separated-values, 17367 data points
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  • 168
    Publication Date: 2023-03-14
    Keywords: Barometric pressure sensor, Setra CS100; Battery terminal voltage; DATE/TIME; Glaciers Austria; HEIGHT above ground; HEK_WST; Hochebenkar; Humidity, relative; Humidity-Temperature probe, Vaisala, HMP45AC; Long-wave downward radiation; Long-wave upward radiation; Net radiometer, Kipp & Zonen, CNR 4; Ötztal, Tyrolian Alps, Austria; Precipitation; Short-wave downward (GLOBAL) radiation; Short-wave upward (REFLEX) radiation; Snow height; Sonic Ranging Sensor, Campbell Scientific, SR50A; Station pressure; Temperature, air; Temperature, technical; Thermometer PT-100, air; Tipping bucket rain gauge, R. M. Young, 52203; Weather station/meteorological observation; Wind direction; Wind monitor, R.M. Young, model 05103; Wind speed; Wind speed, maximum; WST
    Type: Dataset
    Format: text/tab-separated-values, 195828 data points
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  • 169
    Publication Date: 2023-03-14
    Keywords: Barents Sea; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; FN42; FN42_001; FN42_002; FN42_003; FN42_004; FN42_005; FN42_006; FN42_007; FN42_008; FN42_009; FN42_010; FN42_011; FN42_012; FN42_013; FN42_014; FN42_015; FN42_016; FN42_017; FN42_018; FN42_019; FN42_020; FN42_021; FN42_022; FN42_023; FN42_024; FN42_025; FN42_026; FN42_027; FN42_028; FN42_029; FN42_030; FN42_031; FN42_032; FN42_033; FN42_034; FN42_035; FN42_036; FN42_037; FN42_038; FN42_039; FN42_040; FN42_041; FN42_042; FN42_043; FN42_044; FN42_045; FN42_046; FN42_047; FN42_048; FN42_049; FN42_050; FN42_051; FN42_052; FN42_053; FN42_054; FN42_055; FN42_056; FN42_057; FN42_058; FN42_059; FN42_060; FN42_061; FN42_062; FN42_063; FN42_064; FN42_065; FN42_066; FN42_067; FN42_068; FN42_069; FN42_070; FN42_071; FN42_072; FN42_073; FN42_074; FN42_075; FN42_076; FN42_077; FN42_078; FN42_079; FN42_080; FN42_081; FN42_082; FN42_083; FN42_084; FN42_085; FN42_086; FN42_087; FN42_088; FN42_089; FN42_090; FN42_091; FN42_092; FN42_093; FN42_094; FN42_095; FN42_096; FN42_097; FN42_098; FN42_099; FN42_100; FN42_101; FN42_102; FN42_103; FN42_104; FN42_104A; FN42_105; FN42_106; FN42_107; FN42_108; FN42_109; FN42_110; FN42_111; FN42_112; FN42_113; FN42_114; FN42_115; FN42_116; FN42_117; FN42_118; FN42_119; FN42_120; FN42_121; FN42_122; FN42_123; FN42_124; FN42_125; FN42_126; FN42_127; FN42_128; FN42_129; FN42_130; FN42_131; FN42_132; FN42_133; FN42_134; FN42_135; FN42_136; FN42_137; FN42_138; FN42_139; FN42_140; FN42_141; FN42_142; FN42_143; FN42_144; FN42_145; FN42_146; FN42_147; FN42_148; FN42_149; FN42_150; FN42_151; FN42_152; FN42_153; FN42_154; FN42_155; FN42_156; FN42_157; FN42_158; FN42_159; FN42_160; FN42_161; FN42_162; FN42_163; FN42_164; FN42_165; FN42_166; FN42_167; FN42_168; FN42_169; FN42_170; FN42_171; FN42_172; FN42_173; FN42_174; FN42_175; FN42_176; FN42_177; FN42_178; FN42_179; FN42_180; FN42_181; FN42_182; FN42_183; FN42_184; FN42_184A; FN42_185; FN42_186; FN42_186A; FN42_187; FN42_188; FN42_189; FN42_190; FN42_191; FN42_192; FN42_193; FN42_194; FN42_195; FN42_196; FN42_197; FN42_198; FN42_199; FN42_200; FN42_200A; FN42_201; FN42_202; FN42_203; FN42_204; FN42_205; FN42_206; FN42_207; FN42_208; FN42_209; FN42_210; FN42_211; FN42_212; FN42_213; FN42_213A; FN42_214; FN42_214A; FN42_215; FN42_216; FN42_217; FN42_218; FN42_219; FN42_220; FN42_221; FN42_222; FN42_222A; FN42_223; FN42_223A; FN42_224; FN42_225; FN42_226; FN42_227; FN42_228; FN42_228A; FN42_229; FN42_229A; FN42_230; FN42_231; FN42_231A; FN42_232; FN42_233; FN42_234; FN42_235; FN42_236; FN42_237; Fritjof Nansen; Latitude of event; Longitude of event; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus; Salinity; Silicate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 4901 data points
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  • 170
    Publication Date: 2023-03-14
    Keywords: Arsenic; Benthic Chamber; Benthic Flux\Cold1 ExpA; Benthic Flux\Cold1 ExpB; Benthic Flux\Hot1 ExpA; Benthic Flux\Hot1 ExpB; Boron; Bromine; Caesium; Calcium; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; CHAM; Chloride; Chromium; Cobalt; Comment; Copper; DATE/TIME; DEPTH, sediment/rock; ECO2; ECO2-6; ECO2-6-1; ECO2-6-2; ECO2-6-50; ECO2-6-51; Elevation of event; Event label; Hydrogen sulfide; Indium; Inductively coupled plasma - mass spectrometry (ICP-MS); Iodine; Ion chromatography; Iron; Lead; Magnesium; Manganese; Mercury; Nickel; Oxygen; Panarea; pH; pH meter; Potassium; Rubidium; Sample code/label; Sodium; Spectrophotometry; Strontium; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Sulfate; Temperature, water; Tin; Titration, Winkler; Total organic carbon analyzer (TOC-VCPH); Uranium; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 544 data points
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  • 171
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itumbiara; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 1008 data points
    Location Call Number Expected Availability
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  • 172
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; Serra_da_Mesa_reservoir; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 37554 data points
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  • 173
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tucurui_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 2769 data points
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  • 174
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tucurui_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 3043 data points
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  • 175
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Funil_reservoir; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 1854 data points
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  • 176
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itumbiara; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 26152 data points
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  • 177
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itaipu_reservoir; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 26024 data points
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  • 178
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tres_Marias_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 4862 data points
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  • 179
    Publication Date: 2023-03-14
    Keywords: AWI Arctic Land Expedition; Bolshoy Lyakhovsky Island, East Siberia, Russia; Conductivity; Date/Time of event; DEPTH, water; Event label; LAP-01d; LAP-02; LAP-03; LAP-04; LAP-05; LAP-06; LAP-07; LAP-08; LAP-09; LAP-10; LAP-11; LAP-12; LAP-13; LAP-14; LAP-15; LAP-16a; LAP-17; LAP-18; LAP-19; LAP-20; LAP-21; LAP-22; LAP-23; LAP-24; LAP-25; LAP-26; LAP-27; LAP-28; LAP-29; LAP-31; LAP-32; LAP-35; LAP-36; LAP-37; Latitude of event; Lena2007; Location of event; Longitude of event; near Tiksi, East Siberia, Russia; Oyogos Yar, East Siberia, Russia; pH; RU-Land_2007_Lena; Sample code/label; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
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  • 180
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itumbiara; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 23598 data points
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  • 181
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; Serra_da_Mesa_reservoir; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 1842 data points
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  • 182
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tres_Marias_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 2253 data points
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  • 183
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tucurui_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 23417 data points
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  • 184
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Tucurui_reservoir; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 20286 data points
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  • 185
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Itumbiara; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 38574 data points
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  • 186
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Manso_reservoir; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 52687 data points
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  • 187
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Chlorophyll a; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Manso_reservoir; Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 34789 data points
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  • 188
    Publication Date: 2023-03-14
    Keywords: Brazil; BUOY_MET; Conductivity; DATE/TIME; DEPTH, water; Integrated System for Environmental Monitoring (SIMA); Meteorological buoy; Oxygen; pH; SIMA; Temperature, water; Turbidity (Nephelometric turbidity unit); Xingo_reservoir
    Type: Dataset
    Format: text/tab-separated-values, 11895 data points
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  • 189
    Publication Date: 2023-03-14
    Keywords: -; Alkalinity, total; Ammonium; Arsenic; Arsenic, error, relative; Bahamas; Barium; Barium, error, relative; Cadmium, error, relative; Caesium; Caesium, error, relative; Calcium; Calcium, error, relative; Calculated; Carbon, inorganic, dissolved; Carbonate ion; Chromium; Chromium, error, relative; Cobalt; Cobalt, error, relative; Copper; Copper, error, relative; DEPTH, sediment/rock; Description; Exuma; Hydrogen sulfide; ICP-Q-MS; Inductively coupled plasma-quadrupole-mass spectrometry; Iron; Iron, error, relative; Lead; Lead, error, relative; Magnesium; Magnesium, error, relative; Manganese; Manganese, error, relative; Nickel; Nickel, error, relative; Oxygen saturation; pH; Phosphate; Rhenium; Rhenium, error, relative; Rubidium; Rubidium, error, relative; Salinity; Strontium; Strontium, error, relative; Uranium; Uranium, error, relative; Vanadium; Vanadium, error, relative; Wet chemistry; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 2589 data points
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  • 190
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    Unknown
    PANGAEA
    Publication Date: 2023-03-14
    Keywords: Ammonium; BDOG1; BDOG2; BDOG3; Benin, West Africa; Bicarbonate ion; Bromide; Calcium; Calculated; Chloride; Code; Conductivity; DATE/TIME; Depth, groundwater table; Deuterium excess; Dogue-Haus; DRILL; Drilling/drill rig; Event label; FE01; FE02; Fluorine; Global Change and the Hydrological Cycle; GLOWA; GWB1; GWB2; GWB3; ID 1; ID 150; ID 182; ID 183; ID 19; ID 193; ID 194; ID 195; ID 2; ID 204; ID 205; ID 206; ID 207; ID 208; ID 215; ID 216; ID 217; ID 253; ID 260; Identification; IMPETUS; Ionic balance; Iron 2+; Magnesium; Manganese; Nitrate; Nitrite; OW01; OW02; OW03; OW04; OW05; OW06; OW07; OW08; OW09; OW10; Oxidation reduction (RedOx) potential; Oxygen; pH; Phosphate; Potassium; Sample type; Sampling Well; Silica, dissolved; Sodium; Strontium; Sulfate; Surface water sample; SWS; Temperature, water; Water sample; WELL; WS; δ18O; δ Deuterium
    Type: Dataset
    Format: text/tab-separated-values, 2321 data points
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  • 191
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; Calcite saturation state; Calculated; Carbon, inorganic, dissolved; Carbonate ion; Carbon dioxide; Carbon dioxide, partial pressure; CTD/Rosette; CTD-RO; DEPTH, water; Elevation of event; El Puma; Event label; Gulf of California; Latitude of event; Longitude of event; Mediterranean Sea Acidification in a Changing Climate; MedSeA; pH; pH meter (Metrohm ph mobile); Salinity; Temperature, water; WACTD-02-01CTD; WACTD-02-02CTD; WACTD-02-09CTD; WACTD-02-12CTD; WACTD-02-19CTD; WACTD-02-25CTD; WACTD-02-27CTD; WACTD-02-29CTD; WACTD-02-31CTD; WAG-02
    Type: Dataset
    Format: text/tab-separated-values, 97 data points
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  • 192
    Publication Date: 2023-03-14
    Keywords: Carbon, organic, particulate; Carbon, organic, particulate, standard deviation; Conductivity, electrical; Conductivity, standard deviation; DATE/TIME; Date/time end; Lake type; Mackenzie_area; MULT; Multiple investigations; Nitrate and Nitrite; Nitrate and Nitrite, standard deviation; Nitrogen, organic, particulate; Nitrogen, organic, particulate, standard deviation; Nitrogen, standard deviation; Nitrogen, total; Nitrogen, total, standard deviation; Nitrogen, total dissolved; Nitrogen in ammonia; Nitrogen in ammonia, standard deviation; Northwest Territories, Canada; pH; pH, standard deviation; Phosphate; Phosphorus, dissolved; Phosphorus, standard deviation; Phosphorus, total; Temperature, water; Temperature, water, maximum; Temperature, water, minimum; Temperature, water, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 193
    Publication Date: 2023-03-14
    Keywords: Barometric pressure sensor, Setra CS100; Battery terminal voltage; DATE/TIME; Glaciers Austria; HEIGHT above ground; HEK_WST; Hochebenkar; Humidity, relative; Humidity-Temperature probe, Vaisala, HMP45AC; Long-wave downward radiation; Long-wave upward radiation; Net radiometer, Kipp & Zonen, CNR 4; Ötztal, Tyrolian Alps, Austria; Precipitation; Short-wave downward (GLOBAL) radiation; Short-wave upward (REFLEX) radiation; Snow height; Sonic Ranging Sensor, Campbell Scientific, SR50A; Station pressure; Temperature, air; Temperature, technical; Thermometer PT-100, air; Tipping bucket rain gauge, R. M. Young, 52203; Weather station/meteorological observation; Wind direction; Wind monitor, R.M. Young, model 05103; Wind speed; Wind speed, maximum; WST
    Type: Dataset
    Format: text/tab-separated-values, 765072 data points
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  • 194
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lidbury, Ian; Johnson, Vivienne R; Hall-Spencer, Jason M; Munn, Colin B; Cunliffe, Michael (2012): Community-level response of coastal microbial biofilms to ocean acidification in a natural carbon dioxide vent ecosystem. Marine Pollution Bulletin, 64(5), 1063-1066, https://doi.org/10.1016/j.marpolbul.2012.02.011
    Publication Date: 2023-03-14
    Description: The impacts of ocean acidification on coastal biofilms are poorly understood. Carbon dioxide vent areas provide an opportunity to make predictions about the impacts of ocean acidification. We compared biofilms that colonised glass slides in areas exposed to ambient and elevated levels of pCO2 along a coastal pH gradient, with biofilms grown at ambient and reduced light levels. Biofilm production was highest under ambient light levels, but under both light regimes biofilm production was enhanced in seawater with high pCO2. Uronic acids are a component of biofilms and increased significantly with high pCO2. Bacteria and Eukarya denaturing gradient gel electrophoresis profile analysis showed clear differences in the structures of ambient and reduced light biofilm communities, and biofilms grown at high pCO2 compared with ambient conditions. This study characterises biofilm response to natural seabed CO2 seeps and provides a baseline understanding of how coastal ecosystems may respond to increased pCO2 levels.
    Keywords: Alkalinity, total; AS-Alk 2 Total Alkalinity Titrator (Apollo SciTech Inc, Georgia, USA); average; Calculated using CO2SYS; Carbon, inorganic, dissolved; Carbon dioxide, partial pressure; DEPTH, water; EXP; Experiment; Mediterranean Sea Acidification in a Changing Climate; MedSeA; pH; Site; Vulcano; Vulcano, Aeolian Islands, North East Sicily, Italy
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 195
    Publication Date: 2023-03-14
    Keywords: Barometric pressure sensor, Setra CS100; Battery terminal voltage; DATE/TIME; Glaciers Austria; HEIGHT above ground; HEK_WST; Hochebenkar; Humidity, relative; Humidity-Temperature probe, Vaisala, HMP45AC; Long-wave downward radiation; Long-wave upward radiation; Net radiometer, Kipp & Zonen, CNR 4; Ötztal, Tyrolian Alps, Austria; Precipitation; Short-wave downward (GLOBAL) radiation; Short-wave upward (REFLEX) radiation; Snow height; Sonic Ranging Sensor, Campbell Scientific, SR50A; Station pressure; Temperature, air; Temperature, technical; Thermometer PT-100, air; Tipping bucket rain gauge, R. M. Young, 52203; Weather station/meteorological observation; Wind direction; Wind monitor, R.M. Young, model 05103; Wind speed; Wind speed, maximum; WST
    Type: Dataset
    Format: text/tab-separated-values, 586831 data points
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  • 196
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Bottle, Niskin 5-L; bottle/Cratere; Carbon, inorganic, dissolved; Carbon dioxide; Carbon dioxide, partial pressure; Date/Time of event; DEPTH, water; ECO2; ECO2-6; ECO2-6-43; ECO2-6-68; Elevation of event; Event label; Hydrogen sulfide; Latitude of event; Longitude of event; Methane; NIS_5L; Nitrogen, gas; Oxygen; Oxygen, gas; Panarea; pH; pH meter; Salinity; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Titration
    Type: Dataset
    Format: text/tab-separated-values, 79 data points
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  • 197
    Publication Date: 2023-03-16
    Keywords: AWI_GeoPhy; Description; Marine Geophysics @ AWI; Projection; Resolution; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 198
  • 199
    Publication Date: 2023-03-16
    Keywords: Archive of Ocean Data; ARCOD; Ash; Ash mass; Calculated; Ekolog; Ekolog-2002; Ekolog-2002-3aP; Ekolog-2002-58P; Ekolog-2002-76P; Ekolog-2002-78P; Elevation of event; Event label; Latitude of event; Location; Longitude of event; PLA; Plankton net; Sample, dry mass; Weighted; White Sea
    Type: Dataset
    Format: text/tab-separated-values, 16 data points
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  • 200
    Publication Date: 2023-03-16
    Keywords: Archive of Ocean Data; ARCOD; Ash; Ash mass; Calculated; Ekolog; Ekolog-2002; Ekolog-2002-1aP; Ekolog-2002-64P; Ekolog-2002-66P; Elevation of event; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; PLA; Plankton net; Sample, dry mass; Weighted; White Sea
    Type: Dataset
    Format: text/tab-separated-values, 9 data points
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