Sharon Robinson

Prof. Sharon Robinson

orcid

Research Focus & Metrics

Academic Career Length

37Years (1990-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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31 March 2017 in Science
Verified
Journal Article
Closed access
GPGretta T. Pecl
Gretta T. Pecl
MAMiguel B. Araújo
Miguel B. Araújo
JBJohann D. Bell
Johann D. Bell
JBJulia Blanchard
Julia Blanchard
TBTimothy C. Bonebrake
Timothy C. Bonebrake
SWStephen E. Williams
Stephen E. Williams
Consequences of shifting species distributions: Climate change is causing geographical redistribution of plant and animal species globally. These distributional shifts are leading to new ecosystems and ecological communities, changes that will affect human society. Pecl et al. review these current and future impacts and assess their implications for sustainable development goals. Science , this issue p. eaai9214

18 April 2013 in Polar Record
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Journal Article
Open access
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JTJohn Turner
John Turner
NBNicholas E. Barrand
Nicholas E. Barrand
TBThomas J. Bracegirdle
Thomas J. Bracegirdle
PCPeter Convey
Peter Convey
DHDominic A. Hodgson
Dominic A. Hodgson
AKAlexander Klepikov
Alexander Klepikov
We present an update of the ‘key points’ from the Antarctic Climate Change and the Environment (ACCE) report that was published by the Scientific Committee on Antarctic Research (SCAR) in 2009. We summarise subsequent advances in knowledge concerning how the climates of the Antarctic and Southern Ocean have changed in the past, how they might change in the future, and examine the associated impacts on the marine and terrestrial biota. We also incorporate relevant material presented by SCAR to the Antarctic Treaty Consultative Meetings, and make use of emerging results that will form part of the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report.

1 May 2014 in Ecological Monographs
Verified
Journal Article
Closed access
PCPeter Convey
Peter Convey
SCSteven L. Chown
Steven L. Chown
ACAndrew Clarke
Andrew Clarke
DBDavid K. A. Barnes
David K. A. Barnes
SBStef Bokhorst
Stef Bokhorst
DWDiana H. Wall
Diana H. Wall

11 February 2022 in Global Change Biology
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Journal Article
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JLJonas Lembrechts
Jonas Lembrechts
JHJohan van Den Hoogen
Johan van Den Hoogen
JAJuha Aalto
Juha Aalto
MAMichael B. Ashcroft
Michael B. Ashcroft
PFPieter De Frenne
Pieter De Frenne
JLJonathan Lenoir
Jonathan Lenoir
Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1‐km2resolution for 0–5 and 5–15 cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1‐km2pixels (summarized from 8519 unique temperature sensors) across all the world's major terrestrial biomes, and coarse‐grained air temperature estimates from ERA5‐Land (an atmospheric reanalysis by the European Centre for Medium‐Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (−0.7 ± 2.3°C). The observed substantial and biome‐specific offsets emphasize that the projected impacts of climate and climate change on near‐surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil‐related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications.

10 May 2013 in Genome Biology
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Journal Article
Open access
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RMRay Ming
Ray Ming
RVRobert VanBuren
Robert VanBuren
YLYanling Liu
Yanling Liu
MYMei Yang
Mei Yang
Yuepeng HanYuepeng Han
Yuepeng Han
JSJane Shen-Miller
Jane Shen-Miller
Background: Sacred lotus is a basal eudicot with agricultural, medicinal, cultural and religious importance. It was domesticated in Asia about 7,000 years ago, and cultivated for its rhizomes and seeds as a food crop. It is particularly noted for its 1,300-year seed longevity and exceptional water repellency, known as the lotus effect. The latter property is due to the nanoscopic closely packed protuberances of its self-cleaning leaf surface, which have been adapted for the manufacture of a self-cleaning industrial paint, Lotusan. Results: The genome of the China Antique variety of the sacred lotus was sequenced with Illumina and 454 technologies, at respective depths of 101× and 5.2×. The final assembly has a contig N50 of 38.8 kbp and a scaffold N50 of 3.4 Mbp, and covers 86.5% of the estimated 929 Mbp total genome size. The genome notably lacks the paleo-triplication observed in other eudicots, but reveals a lineage-specific duplication. The genome has evidence of slow evolution, with a 30% slower nucleotide mutation rate than observed in grape. Comparisons of the available sequenced genomes suggest a minimum gene set for vascular plants of 4,223 genes. Strikingly, the sacred lotus has 16 COG2132 multi-copper oxidase family proteins with root-specific expression; these are involved in root meristem phosphate starvation, reflecting adaptation to limited nutrient availability in an aquatic environment. Conclusions: The slow nucleotide substitution rate makes the sacred lotus a better resource than the current standard, grape, for reconstructing the pan-eudicot genome, and should therefore accelerate comparative analysis between eudicots and monocots.

28 May 2014 in Nature Climate Change
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Journal Article
Open access
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CWCraig E. Williamson
Craig E. Williamson
RZRichard G. Zepp
Richard G. Zepp
RLRobyn Lucas
Robyn Lucas
SMSasha Madronich
Sasha Madronich
AAAmy T. Austin
Amy T. Austin
JBJanet F Bornman
Janet F Bornman
The projected large increases in damaging ultraviolet radiation as a result of global emissions of ozone-depleting substances have been forestalled by the success of the Montreal Protocol. New challenges are now arising in relation to climate change. We highlight the complex interactions between the drivers of climate change and those of stratospheric ozone depletion, and the positive and negative feedbacks among climate, ozone and ultraviolet radiation. These will result in both risks and benefits of exposure to ultraviolet radiation for the environment and human welfare. This Review synthesizes these new insights and their relevance in a world where changes in climate as well as in stratospheric ozone are altering exposure to ultraviolet radiation with largely unknown consequences for the biosphere.