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| 62. |
- Hanson, M. L., et al.
(författare)
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How we can make ecotoxicology more valuable to environmental protection
- 2017
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Ingår i: Science of the Total Environment. - : Elsevier BV. - 0048-9697 .- 1879-1026. ; 578, s. 228-235
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Tidskriftsartikel (refereegranskat)abstract
- There is increasing awareness that the value of peer-reviewed scientific literature is not consistent, resulting in a growing desire to improve the practice and reporting of studies. This is especially important in the field of ecotoxicology, where regulatory decisions can be partly based on data from the peer-reviewed literature, with wide-reaching implications for environmental protection. Our objective is to improve the reporting of ecotoxicology studies so that they can be appropriately utilized in a fair and transparent fashion, based on their reliability and relevance. We propose a series of nine reporting requirements, followed by a set of recommendations for adoption by the ecotoxicology community. These reporting requirements will provide clarity on the the test chemical, experimental design and conditions, chemical identification, test organisms, exposure confirmation, measurable endpoints, how data are presented, data availability and statistical analysis. Providing these specific details will allow for a fuller assessment of the reliability and relevance of the studies, including limitations. Recommendations for the implementation of these reporting requirements are provided herein for practitioners, journals, reviewers, regulators, stakeholders, funders, and professional societies. If applied, our recommendations will improve the quality of ecotoxicology studies and their value to environmental protection.
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| 63. |
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| 64. |
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| 65. |
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| 66. |
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| 67. |
- Miller, Rachael, et al.
(författare)
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Socio-ecological correlates of neophobia in corvids
- 2022
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Ingår i: Current Biology. - : Elsevier BV. - 0960-9822. ; 32:1, s. 4-85
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Tidskriftsartikel (refereegranskat)abstract
- Behavioral responses to novelty, including fear and subsequent avoidance of novel stimuli, i.e., neophobia, determine how animals interact with their environment. Neophobia aids in navigating risk and impacts on adaptability and survival. There is variation within and between individuals and species; however, lack of large-scale, comparative studies critically limits investigation of the socio-ecological drivers of neophobia. In this study, we tested responses to novel objects and food (alongside familiar food) versus a baseline (familiar food alone) in 10 corvid species (241 subjects) across 10 labs worldwide. There were species differences in the latency to touch familiar food in the novel object and novel food conditions relative to the baseline. Four of seven socio-ecological factors influenced object neophobia: (1) use of urban habitat (versus not), (2) territorial pair versus family group sociality, (3) large versus small maximum flock size, and (4) moderate versus specialized caching (whereas range, hunting live animals, and genus did not), while only maximum flock size influenced food neophobia. We found that, overall, individuals were temporally and contextually repeatable (i.e., consistent) in their novelty responses in all conditions, indicating neophobia is a stable behavioral trait. With this study, we have established a network of corvid researchers, demonstrating potential for further collaboration to explore the evolution of cognition in corvids and other bird species. These novel findings enable us, for the first time in corvids, to identify the socio-ecological correlates of neophobia and grant insight into specific elements that drive higher neophobic responses in this avian family group. Video abstract: [Figure presented]
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| 68. |
- Roethlisberger, R., et al.
(författare)
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The Southern Hemisphere at glacial terminations : insights from the Dome C ice core
- 2008
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Ingår i: Climate of the past. - : Copernicus GmbH. - 1814-9324 .- 1814-9332. ; 4:4, s. 345-356
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Tidskriftsartikel (refereegranskat)abstract
- The many different proxy records from the European Project for Ice Coring in Antarctica (EPICA) Dome C ice core allow for the first time a comparison of nine glacial terminations in great detail. Despite the fact that all terminations cover the transition from a glacial maximum into an interglacial, there are large differences between single terminations. For some terminations, Antarctic temperature increased only moderately, while for others, the amplitude of change at the termination was much larger. For the different terminations, the rate of change in temperature is more similar than the magnitude or duration of change. These temperature changes were accompanied by vast changes in dust and sea salt deposition all over Antarctica. Here we investigate the phasing between a South American dust proxy (non-sea-salt calcium flux, nssCa(2+)), a sea ice proxy (sea salt sodium flux, ssNa(+)) and a proxy for Antarctic temperature (deuterium, delta D). In particular, we look into whether a similar sequence of events applies to all terminations, despite their different characteristics. All proxies are derived from the EPICA Dome C ice core, resulting in a relative dating uncertainty between the proxies of less than 20 years. At the start of the terminations, the temperature (delta D) increase and dust (nssCa(2+) flux) decrease start synchronously. The sea ice proxy (ssNa(+) flux), however, only changes once the temperature has reached a particular threshold, approximately 5 degrees C below present day temperatures (corresponding to a delta D value of -420 parts per thousand). This reflects to a large extent the limited sensitivity of the sea ice proxy during very cold periods with large sea ice extent. At terminations where this threshold is not reached (TVI, TVIII), ssNa(+) flux shows no changes. Above this threshold, the sea ice proxy is closely coupled to the Antarctic temperature, and interglacial levels are reached at the same time for both ssNa(+) and delta D. On the other hand, once another threshold at approximately 2 degrees C below present day temperature is passed (corresponding to a delta D value of -402 parts per thousand), nssCa(2+) flux has reached interglacial levels and does not change any more, despite further warming. This threshold behaviour most likely results from a combination of changes to the threshold friction velocity for dust entrainment and to the distribution of surface wind speeds in the dust source region.
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| 69. |
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