Wetlands provide ∼$47.4 trillion/year worth of ecosystem services globally and support immense biodiversity, yet face widespread drainage and pollution, and large-scale wetlands restoration is urgentl
The findings support the possibility that FBOM-δ13C can be used as a paleoceanographic proxy for surface water [CO2(aq)] and thus atmospheric pCO2.
This chapter aligns with Goal 14: Life Below Water and Goal 13: Climate Action by highlighting how past marine ecosystem changes can improve our understanding of future climactic and chemical conditions of global oceans.
Elsevier,

Ocean Currents, Physical Drivers in a Changing World, 2021, Pages 497-520

This book chapter advances SDG 14 by explaining how ocean currents further influence climate via freshwater transports that influence dense water formation at high latitudes. Under a warming climate and an intensifying hydrological cycle, ocean currents convey salinity anomalies that could destabilize the circulation.
Elsevier, Current Opinion in Green and Sustainable Chemistry, Volume 29, June 2021
This review is dedicated to ecocatalysis, a concept developed by the Grison group aiming at combining ecology and green chemistry, which could be the vector of sustainable development based on the pri
Elsevier, Case Studies in Chemical and Environmental Engineering, Volume 3, June 2021
The widespread consumption of electronic devices has made spent batteries an ongoing economic and ecological concern with a compound annual growth rate of up to 8% during 2018, and expected to reach b
Quantification and extent mapping of seawater intrusive zones are extremely critical for coastal aquifers, especially for those impacted with anthropogenic stress.
After 10 years of the Fukushima Nuclear Accident, Japan decided on 13 April 2021 to release the nuclear wastewater into the Pacific Ocean.
The recent Intergovernmental Panel on Climate Change (IPCC) Special Report on Oceans and the Cryosphere in a Changing Climate suggests sea level rise may be best understood as a slow onset disaster fo
This paper reviews the evidence on slow-onset events presented in the Special Report on Climate Change and Land (SRCCL) and the Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC)

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