JC Ellison

ORCID: 0000-0003-0692-8347
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Research Areas
  • Coastal wetland ecosystem dynamics
  • Coastal and Marine Dynamics
  • Geology and Paleoclimatology Research
  • Pacific and Southeast Asian Studies
  • Climate Change, Adaptation, Migration
  • Geological formations and processes
  • Coastal and Marine Management
  • Marine and coastal plant biology
  • Geological and Geophysical Studies
  • Coral and Marine Ecosystems Studies
  • Isotope Analysis in Ecology
  • Oil Palm Production and Sustainability
  • Marine and fisheries research
  • Aeolian processes and effects
  • Electrochemical Analysis and Applications
  • Hydrology and Watershed Management Studies
  • Tropical and Extratropical Cyclones Research
  • Soil erosion and sediment transport
  • Indigenous Studies and Ecology
  • Conservation, Biodiversity, and Resource Management
  • Hydrology and Sediment Transport Processes
  • Echinoderm biology and ecology
  • Climate change impacts on agriculture
  • Marine Bivalve and Aquaculture Studies
  • Island Studies and Pacific Affairs

University of Tasmania
2015-2024

University of Oxford
2013-2015

Oxfam
2015

Cornell University
2005

Queen's Medical Centre
2005

University of Leicester
2000

Australian National University
1994-1998

Australian Institute of Marine Science
1998

The University of Queensland
1998

University of California, Berkeley
1991-1993

Mangrove species are uniquely adapted to tropical and subtropical coasts, although relatively low in number of species, mangrove forests provide at least US $1.6 billion each year ecosystem services support coastal livelihoods worldwide. Globally, areas declining rapidly as they cleared for development aquaculture logged timber fuel production. Little is known about the effects area loss on individual local or regional populations. To address this gap, species-specific information global...

10.1371/journal.pone.0010095 article EN cc-by PLoS ONE 2010-04-08

Numerous factors affect the distribution of mangrove plants.Most species are typically dispersed by.water-buoyant propagules, allowing them to take advantage estuarine, coastal and ocean currents both replenish existing stands establish new ones.The direction they travel depends on sea land barriers, but dispersal distance time that propagules remain buoyant viable.This is expected differ for each species.Similarly, will also in establishment success growth development rate, has tolerance...

10.2307/2997695 article EN Global Ecology and Biogeography Letters 1998-01-01

Davidson, J. L., C. Jacobson, A. Lyth, Dedekorkut-Howes, L. Baldwin, Ellison, N. Holbrook, M. Howes, S. Serrao-Neumann, Singh-Peterson, and T. F. Smith. 2016. Interrogating resilience: toward a typology to improve its operationalization. Ecology Society 21(2):27.http://dx.doi.org/10.5751/ES-08450-210227

10.5751/es-08450-210227 article EN cc-by Ecology and Society 2016-01-01

Climate change, particularly its associated sea level rise, is major threat to mangrove coastal areas, and it essential develop ways reduce vulnerability through strategic management planning. Vulnerability has three dimensions of exposure stresses, sensitivity, related adaptive capacity, measure components each were trialled at sites in Africa the South Pacific an analysis procedure based on ranking. The approaches ranking system for assessment systems integrate biotic abiotic factors along...

10.1007/s11273-014-9397-8 article EN cc-by Wetlands Ecology and Management 2014-12-30

10.1006/ecss.1993.1042 article EN Estuarine Coastal and Shelf Science 1993-07-01

10.1016/s0025-326x(98)00122-2 article EN Marine Pollution Bulletin 1999-12-01

We present the basis for an entirely new approach to in situ nanoparticle sizing. Nanoparticles containing just 12 zeptomoles (1 zeptomole = 10(-21) moles) of silver, are detected via particle coulometry. These stochastic charge measurements correspond transfer only 7000-8000 electrons, yielding direct information relating individual volumes. The resulting size distribution (average equivalent radius 5 nm) obtained coulometry is excellent correspondence with that attained from TEM analysis....

10.1039/c5an00474h article EN The Analyst 2015-01-01

Tidal marshes store large amounts of organic carbon in their soils. Field data quantifying soil (SOC) stocks provide an important resource for researchers, natural managers, and policy-makers working towards the protection, restoration, valuation these ecosystems. We collated a global dataset tidal marsh (MarSOC) from 99 studies that includes location, depth, site name, dry bulk density, SOC, and/or matter (SOM). The MarSOC 17,454 points 2,329 unique locations, 29 countries. generated...

10.1038/s41597-023-02633-x article EN cc-by Scientific Data 2023-11-11

Not every first footstep on a virgin shore leaves enduring trace, nor human settlement an deposit that chances to survive, and then be observed archaeologically. Good environmental evidence from Mangaia Island, central East Polynesia, gives — it is contended fairer picture of the invasion remote Oceania than short sceptical chronology recently published in ANTIQUITY.

10.1017/s0003598x00046615 article EN Antiquity 1994-06-01

Intertidal mangrove ecosystems are sensitive to climate change impacts, particularly associated relative sea level rise. Human stressors and low tidal range add vulnerability, both characteristics of the Doula Estuary, Cameroon. To investigate spatial techniques were combined with ground surveys map distributions zones, compare historical records quantify over last few decades. Low technology used establish elevation mapped area. Stratigraphic coring palaeobiological reconstruction show...

10.3390/biology1030617 article EN cc-by Biology 2012-11-06

Abstract Anodic particle coloumetry is used to size silver nanoparticles impacting a carbon microelectrode in potassium chloride/citrate solution. Besides their size, agglomeration state solution also investigated solely by electrochemical means and subsequent data analysis. Validation of this new approach nanoparticle studies performed comparison with the results commercially available tracking analysis system, which shows excellent agreement. Moreover, it demonstrated that technique has...

10.1002/open.201300005 article EN cc-by-nc-nd ChemistryOpen 2013-03-15

Geodiversity assessment is recent and passing through a stage of methodological development consolidation. With rapid environmental change, improving the developmental states geodiversity paramount importance. A scientometric analysis presented to identify knowledge gaps, current trends avenues for future research in quantitative literature. The study categorised into three areas analysis: (a) intentions assessment, (b) methods (c) geographic trends. ranking tool was developed determine...

10.1177/0309133320967219 article EN Progress in Physical Geography Earth and Environment 2020-11-11

10.1016/0031-0182(89)90068-0 article EN Palaeogeography Palaeoclimatology Palaeoecology 1989-11-01

CR Climate Research Contact the journal Facebook (Twitter) RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout JournalEditorsSpecials 32:161-176 (2006) - doi:10.3354/cr032161 Adapting Pacific Island mangrove responses sea level rise and climate change Eric L. Gilman1,15,*, Joanna Ellison1, Vainuupo Jungblut2, Hanneke Van Lavieren3, Lisette Wilson4, Francis Areki5, Genevieve Brighouse6, John Bungitak7, Eunice Dus8, Marion Henry9, Mandes Kilman10, Elizabeth...

10.3354/cr032161 article EN Climate Research 2006-10-26

10.1016/j.palaeo.2005.01.008 article EN Palaeogeography Palaeoclimatology Palaeoecology 2005-04-08

Flood frequency analysis using partial series data has been shown to provide better estimates of small medium magnitude flood events than the annual series, but is more often employed due its simplicity. Where average recurrence intervals are required, values “converted” Langbein equation, regardless whether statistical assumptions behind equation fulfilled. This study uses from Northern Tasmanian stream-gauging stations make empirical comparisons between and provided by equation. At T = 1.1...

10.3390/w5041816 article EN Water 2013-11-18
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