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  • 2015-2019  (2,132)
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  • 1
    Call number: RIFS 23.95559
    Description / Table of Contents: A cutting exploration of how cities drive climate change while being on the frontlines of the coming climate crisis. How will climate change affect our lives? Where will its impacts be most deeply felt? Are we doing enough to protect ourselves from the coming chaos? In Extreme Cities, Ashley Dawson argues that cities are ground zero for climate change, contributing the lion’s share of carbon to the atmosphere, while also lying on the frontlines of rising sea levels. Today, the majority of the world’s megacities are located in coastal zones, yet few of them are adequately prepared for the floods that will increasingly menace their shores. Instead, most continue to develop luxury waterfront condos for the elite and industrial facilities for corporations. These not only intensify carbon emissions, but also place coastal residents at greater risk when water levels rise. In Extreme Cities, Dawson offers an alarming portrait of the future of our cities as varied as Jakarta, Dehli, Port-au-Prince and Sao Paulo, describing the efforts of Staten Island, New York, and Shishmareff, Alaska residents to relocate; Holland’s models for defending against the seas; and the development of New York City before and after Hurricane Sandy. Our best hope lies not with fortified sea walls, he argues. Rather, it lies with urban movements already fighting to remake our cities in a more just and equitable way.
    Type of Medium: Monograph available for loan
    Pages: v, 378 Seiten , Illustrationen
    ISBN: 9781784780364
    Language: English
    Note: Introduction: extreme city , Capital sinks , Environmental blowback , Sea change , The jargon of resilience , Climate apartheid , Disaster communism , Conclusion: urban futures
    Branch Library: RIFS Library
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  • 2
    Publication Date: 2023-10-07
    Description: This data set presents 374 organizations providing Polar specific weather, water, ice and climate information. The organizations are categorized in different categories and classes based on their base country, institutional characteristics and targeted users.
    Keywords: climate; environmental information providers; ice; Polar Regions; water; weather; Year of Polar Prediction; YOPP
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 47 kBytes
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  • 3
    Publication Date: 2024-02-10
    Keywords: anoxygenic phototrophy; brackish coastal ecosystem; CRISPR-Cas; Green sulfur bacteria; microbial bloom; Microbial succession; Microviridae; Prosthecochloris; resilience; RIVER; Sampling river; Trunk_River_Woods_Hole; Virus; Woods Hole, USA
    Type: Dataset
    Format: application/zip, 289 kBytes
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  • 4
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    In:  Supplement to: Bhatnagar, Srijak; Cowley, Elise S; Kopf, Sebastian; Pérez Castro, Sherlynette; Kearney, Sean; Dawson, Scott C; Hanselmann, Kurt; Ruff, S Emil (2020): Microbial community dynamics and coexistence in a sulfide-driven phototrophic bloom. Environmental Microbiome, 15(1), https://doi.org/10.1186/s40793-019-0348-0
    Publication Date: 2024-02-10
    Description: Organic-rich, brackish water bodies are common along coastlines and important for the biogeochemical cycling of carbon, nitrogen, sulfur, and phosphorus. These ecosystems are dynamic and frequently disturbed by weather, tides, erosion, and human activities. Here, we investigated a shallow, brackish lagoon (Trunk River, Woods Hole, MA) that contains layers of decaying organic matter, which releases hydrogen sulfide upon physical disturbance. To study the microbial habitat and community response to perturbations, we carried out replicated in situ experiments, analyzing the physicochemistry and microbial community succession. At each site, yellow blooms of microorganisms formed within three days after disturbance. The water column changed substantially, establishing steep gradients of temperature, oxygen, sulfide, and salinity. The diverse microbial community at early timepoints was replaced by a community largely dominated by a clonal population of green sulfur bacteria (GSB) Prosthecochloris vibrioformis. Despite its dominance, this population coexisted with less abundant GSBs affiliating with Chlorobaculum. This population represents a new Chlorobaculum species, as indicated by phylogenetic and phylogenomic placement, ANI values, and CRISPR-Cas genes. Interestingly, despite their dominance the GSB coexisted with purple sulfur bacteria (Halochromatium sp. and Allochromatium sp.), anoxygenic phototrophic Chloroflexi (Chloroploca sp.) and other phototrophs. A high relative sequence abundance of Microviridae viruses was found in the metagenome, indicating their activity in the bloom. After two weeks the bloom subsided and the ecosystem slowly returned towards a diverse state and ecosystem functions, indicating its resilience after disturbance. This work provides insights into the assembly, succession, and coexistence of oxygenic and anoxygenic phototrophs in a common coastal ecosystem. The transient bloom was spatially structured analogous to a phototrophic microbial mat with distinct ecological niches for multiple clades of Cyanobacteria, purple and green sulfur bacteria. We suggest that a cryptic sulfur cycle in the water column between sulfur-oxidizing phototrophs, sulfate reducers, and sulfur oxidizers enhanced the development of the bloom. The bloom was likely driven by new species in the order Chlorobiales and possibly impacted by viruses of the family Microviridae.
    Keywords: Acetate; Ammonium; anoxygenic phototrophy; Biomass; brackish coastal ecosystem; Bromide; Calcium; Chloride; Comment; CRISPR-Cas; DATE/TIME; Density; DEPTH, water; Fluoride; Formate; Green sulfur bacteria; High Performance Liquid Chromatography (HPLC); Iron; Iron 2+; Iron 3+; Lactate; Lithium; Magnesium; microbial bloom; Microbial succession; Microviridae; Nitrate; Nitrite; Normalized; Oxygen; pH; Phosphate; Potassium; Present weather; Prosthecochloris; Refractometer; resilience; RIVER; Salinity; Sample ID; Sampling river; Sodium; Succinate; Sulfate; Sulfide, total; Temperature, water; Trunk_River_Woods_Hole; Virus; Water bodies; Woods Hole, USA
    Type: Dataset
    Format: text/tab-separated-values, 3766 data points
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  • 5
    Publication Date: 2018-01-31
    Description: Mutations in LRRK2 are known to be the most common genetic cause of sporadic and familial Parkinson’s disease (PD). Multiple lines of LRRK2 transgenic or knockin mice have been developed, yet none exhibit substantial dopamine (DA)-neuron degeneration. Here we develop human tyrosine hydroxylase (TH) promoter-controlled tetracycline-sensitive LRRK2 G2019S (GS) and LRRK2 G2019S kinase-dead (GS/DA) transgenic mice and show that LRRK2 GS expression leads to an age- and kinase-dependent cell-autonomous neurodegeneration of DA and norepinephrine (NE) neurons. Accompanying the loss of DA neurons are DA-dependent behavioral deficits and α-synuclein pathology that are also LRRK2 GS kinase-dependent. Transmission EM reveals that that there is an LRRK2 GS kinase-dependent significant reduction in synaptic vesicle number and a greater abundance of clathrin-coated vesicles in DA neurons. These transgenic mice indicate that LRRK2-induced DA and NE neurodegeneration is kinase-dependent and can occur in a cell-autonomous manner. Moreover, these mice provide a substantial advance in animal model development for LRRK2-associated PD and an important platform to investigate molecular mechanisms for how DA neurons degenerate as a result of expression of mutant LRRK2.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 6
    Publication Date: 2015-08-31
    Description: Mutations in parkin lead to early-onset autosomal recessive Parkinson’s disease (PD) and inactivation of parkin is thought to contribute to sporadic PD. Adult knockout of parkin in the ventral midbrain of mice leads to an age-dependent loss of dopamine neurons that is dependent on the accumulation of parkin interacting substrate (PARIS), zinc finger protein 746 (ZNF746), and its transcriptional repression of PGC-1α. Here we show that adult knockout of parkin in mouse ventral midbrain leads to decreases in mitochondrial size, number, and protein markers consistent with a defect in mitochondrial biogenesis. This decrease in mitochondrial mass is prevented by short hairpin RNA knockdown of PARIS. PARIS overexpression in mouse ventral midbrain leads to decreases in mitochondrial number and protein markers and PGC-1α–dependent deficits in mitochondrial respiration. Taken together, these results suggest that parkin loss impairs mitochondrial biogenesis, leading to declining function of the mitochondrial pool and cell death.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Publication Date: 2018-01-08
    Description: Accumulating evidence suggests that α-synuclein (α-syn) occurs physiologically as a helically folded tetramer that resists aggregation. However, the mechanisms underlying the regulation of formation of α-syn tetramers are still mostly unknown. Cellular membrane lipids are thought to play an important role in the regulation of α-syn tetramer formation. Since glucocerebrosidase 1 (GBA1) deficiency contributes to the aggregation of α-syn and leads to changes in neuronal glycosphingolipids (GSLs) including gangliosides, we hypothesized that GBA1 deficiency may affect the formation of α-syn tetramers. Here, we show that accumulation of GSLs due to GBA1 deficiency decreases α-syn tetramers and related multimers and increases α-syn monomers in CRISPR-GBA1 knockout (KO) SH-SY5Y cells. Moreover, α-syn tetramers and related multimers are decreased in N370S GBA1 Parkinson’s disease (PD) induced pluripotent stem cell (iPSC)-derived human dopaminergic (hDA) neurons and murine neurons carrying the heterozygous L444P GBA1 mutation. Treatment with miglustat to reduce GSL accumulation and overexpression of GBA1 to augment GBA1 activity reverse the destabilization of α-syn tetramers and protect against α-syn preformed fibril-induced toxicity in hDA neurons. Taken together, these studies provide mechanistic insights into how GBA1 regulates the transition from monomeric α-syn to α-syn tetramers and multimers and suggest unique therapeutic opportunities for PD and dementia with Lewy bodies.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 8
    Publication Date: 2015-04-09
    Description: The aim of this study is to discuss and to extend the characterization of (palaeo)tsunami deposits, and their source materials, based upon the detailed study of their heavy mineral assemblages. Results obtained from three distinct locations (Portugal, Scotland and Indonesia), different coastal contexts and chronologies (the tsunami events studied took place at 1500 cal. yr BP, AD 1755 and 2004) are summarized and discussed in order to contribute to the sedimentological study of onshore (palaeo)tsunami deposits. Results indicate that heavy mineral assemblages primarily reflect local specific conditions. For example, in the Portuguese sites, ca. 90% of the heavy mineral population consists of tourmaline+andalusite+staurolite, whereas in the Scottish samples garnet+amphiboles can be dominant in 90% of the assemblage, where at the Indonesian study site amphiboles+andalusite were the most frequent minerals. The application of Principal Component Analysis for each site reveals that the first two components explain at least 55% of the total variance. In the three studied areas, hydraulic sorting by density was observed and a higher presence of the denser heavy minerals of the assemblages was detected. However, it is important to stress that the sediment source plays a key role in the establishment of the heavy mineral assemblages of the (palaeo)tsunami deposits. In this study, relationships between the likely source sediments and the (palaeo)tsunami deposits were described and whenever possible sediment sources were clearly identified. Furthermore, it was also possible to detect the backwash signal using the analysis of the heavy minerals (e.g. higher frequency of denser minerals or variation in the presence of rounded or euhedral zircon). The work presented here, in contributing to the enhancement of sedimentological criteria presently available to recognize and differentiate extreme marine inundation deposits, also highlights new areas for future research.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 9
    Publication Date: 2015-09-16
    Description: Mutations in parkin lead to early-onset autosomal recessive Parkinson’s disease (PD) and inactivation of parkin is thought to contribute to sporadic PD. Adult knockout of parkin in the ventral midbrain of mice leads to an age-dependent loss of dopamine neurons that is dependent on the accumulation of parkin interacting substrate...
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 10
    Publication Date: 2019
    Description: Abstract The Shetland Isles represent an ideal field laboratory for tsunami geoscience research. This is due to the widespread preservation of Holocene tsunami sediments in coastal peat deposits. This study uses published accounts of the Holocene Storegga Slide tsunami to illustrate how two different approaches – mapping of tsunami sediments and numerical modelling – produce radically different run‐up heights. The Storegga Slide is one of the world largest submarine slides and took place ca 8150 cal yr BP on the continental slope west of Norway. The tsunami generated by the landslide deposited locally extensive sheets of marine sand and gravel, as well as redeposited clasts of peat across the contemporary land surface. These sediment accumulations have subsequently been buried by peat growth during the Holocene while exposures of the deposits are locally visible in coastal cliff sections. In several areas, the tsunami sediments can be traced upslope and inland within the peat as tapering sediment wedges up to maximum altitudes of between ca 8·1 m and 11·8 m above present sea level. Since reconstructions of palaeo‐sea level for Shetland for ca 8150 cal yr BP suggest an altitude of 20 m below high tide on the day that the tsunami struck, it has been inferred that the minimum tsunami run‐up was locally between 28·1 m (8·1 + 20 m) and 31·8 m (11·8 + 20 m). However, numerical models of the tsunami for Shetland suggest that the wave height may only have reached a highest altitude in the order of +13 m above sea level on the day the tsunami took place. In this paper a description is given of the sedimentary evidence for tsunami run‐up in the Shetland Isles. This is followed by an evaluation of where the palaeo‐sea level was located when the tsunami occurred. Significant differences are highlighted in tsunami inundation estimates between those based on the observed (geological) data and the theoretically‐modelled calculations. This example from the Shetland Isles may have global significance since it exemplifies how two different approaches to the reconstruction of tsunami inundation at the coast can produce radically different results with modelled wave height at the coast being considerably less than the geological estimates of tsunami run‐up. This article is protected by copyright. All rights reserved.
    Print ISSN: 0037-0746
    Electronic ISSN: 1365-3091
    Topics: Geosciences
    Published by Wiley
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