You are here: / news homepage

Do you NAWRAS ?

, , ,

The NAWRAS project, coordinated by IRD (Marie BONNIN) and the University of Cadi Ayyad in Marrakech (Jihad ZAHIR), is a research project that proposes to use artificial intelligence to analyze “where, when and how the law protects the oceans.” The goal is to use language models (such as Chat GPT) and train them on texts of marine environmental law in order to obtain indicators that can evaluate the level of legislative protection of the Ocean.

On November 28 and 29, the second seminar of the project was held in Marrakech. On this occasion, two films were made to introduce you to this innovative project and the methods it explores.

 

Project Presentation Video

The 2023 workshop in Marrakech

/by

NAWRAS Project: Workshop on Developing Legal Indicators

, , , ,

Developing Legal Indicators in Environmental Law

The working meeting on legal indicators as part of the Nawras project was held on March 18 and 19, 2024, in the Meeting Room of the Jabir Center / Department of Computer Science of the Faculty of Sciences Semlalia (Cadi Ayyad University – Marrakech).

The 20 participants were able to attend a presentation by Professor Michel Prieur on the importance of developing legal indicators in environmental law. Christophe Bastin then presented the method developed by the International Center for Comparative Environmental Law (CIDCE). The progress of the Nawras project was then presented by Marie Bonnin, Jihad Zahir and Youssef Al Mouatamid. During the next two half-days, the participants debated with the invited researchers (Thais Nunnez-Rocha – environmental economist – University of Orléans, Adrien Comte – IRD LEMAR in visio and Sophie Lanco – IRD Marbec in visio) on the variables and metrics selected as part of the project and on the possibilities of joint publications.

/by

Temporal monitoring of mercury concentrations in tuna, the work of Anaïs Médieu in the press

, ,

The work of Anaïs Medieu on the temporal monitoring of mercury concentrations in tuna has recently been the subject of numerous articles in the national and international press:

As not all of these publications are open access, here is a summary of Anaïs’s results.

The stability of mercury concentrations in tuna since 1971 reflects the inertia of the oceans and calls for massive reductions in emissions to achieve the objectives of the Minamata Convention.

Humans are exposed to toxic methylmercury mainly by consuming marine fish that bioaccumulate methylmercury in the oceans. The Minamata Convention on Mercury of the UN aims to reduce human exposure to mercury through the reduction of anthropogenic emissions. But has this reduction effort led to a reduction in methylmercury concentrations in the oceans and marine fish? An international team of researchers, coordinated by IRD, addressed this question by compiling nearly 3000 mercury measurements in tuna samples captured between 1971 and 2022 in the Pacific, Indian and Atlantic Oceans.

The study reveals that mercury concentrations in tuna have remained globally stable since 1971, except in the northwest Pacific where they significantly increased at the end of the 1990s, probably in connection with the massive increase in anthropogenic emissions associated with the intensive use of fossil fuels for electricity production in Asia. Elsewhere, the stability of mercury levels in tuna does not reflect the global decrease in mercury levels in the atmosphere resulting from emission reduction policies. The researchers attribute this stability in tuna to the inertia of the oceans and the stock of mercury historically emitted that continues to feed the surface or subsurface waters where tuna live. This mercury was emitted decades, if not centuries ago, and does not yet reflect the effects of emission reductions in the atmosphere.

The researchers also simulated the impact of different emission reduction policies on mercury levels in the oceans. Even the strictest emission policy would take 10 to 25 years to initiate a decrease in mercury concentrations in the oceans. These results highlight the need for a global effort to achieve the objectives of the Minamata Convention to reduce emissions and call for continued and long-term global monitoring of mercury levels in marine life.

 

/by

Hydrothermal mercury: the natural history of a contaminant

, ,

Our colleague Hélène Planquette participated in an international study coordinated by the CNRS aiming to estimate the contribution of hydrothermal sources to the mercury stock present in the oceans.

This study has just been published in the journal Nature Geoscience and is the subject of a CNRS press release:

An international team of researchers, coordinated by the CNRS (see inset), has established the first global estimate of hydrothermal mercury (Hg) emissions from mid-ocean ridges. The UN Minamata Convention on Mercury aims to reduce human exposure to toxic mercury by reducing anthropogenic emissions. We are primarily exposed through the consumption of fish that bioaccumulate Hg from the ocean. The current paradigm is that anthropogenic mercury emissions (currently 3,100 tons per year) are responsible for a 21% increase in the global oceanic mercury reservoir. This estimate is inaccurate because we do not know how much natural mercury was present in the ocean before the start of anthropogenic emissions.

We are also unable to quantify the impact of anthropogenic emissions on Hg levels in fish. Hydrothermalism is the only direct source of natural Hg to the ocean. Previous studies, based solely on hydrothermal fluid measurements, suggested that hydrothermal Hg inputs could range from 20 to 2,000 tons per year. This new study used measurements of hydrothermal plumes, seawater, and rock cores in addition to fluid measurements from the Trans-Atlantic Geotraverse (TAG) hydrothermal source on the Mid-Atlantic Ridge.

The combination of observations suggests that the majority of enriched Hg in the fluids would be diluted in seawater, and a small fraction would precipitate locally. Extrapolation of the results indicates that the overall hydrothermal Hg flux from mid-ocean ridges is low (1.5 to 65 tons per year) compared to anthropogenic Hg emissions. Although this suggests that the majority of Hg in the ocean is of anthropogenic origin, it also raises hope that strict implementation of emission reductions under the Minamata Convention will reduce mercury levels in fish and human exposure.

 

Article Reference:

Torres-Rodriguez, N., Yuan, J., Petersen, S. et al. Mercury fluxes from hydrothermal venting at mid-ocean ridges constrained by measurements. Nat. Geosci. (2023).

/by

The ocean may be storing more carbon than estimated in previous studies

, , , ,

Our colleague Frédéric Le Moigne contributed to an international study on the efficiency of the oceanic carbon pump. The study, published this week in Nature magazine, reassesses the ocean’s capacity to store carbon, particularly through ‘marine snow’. The CNRS issued a press release about this publication :

The ocean’s capacity to store atmospheric carbon dioxide is almost 20% higher than the estimates presented in the latest IPCC report. These are the findings of a study published in the journal Nature on 6 December 2023 by an international team including a biologist from the CNRS. The scientists looked at the role played by plankton in the natural transport of carbon from the surface to the seabed.

Plankton is fond of this gas, which it transforms into organic tissue through photosynthesis during its development, and some of it is transformed into marine particles at the end of its life. Denser than seawater, this ‘marine snow’ sinks to the seabed, storing carbon and providing essential nutrients for many deep-sea creatures, from tiny bacteria to deep-sea fish.

Based on the study of a database collected from around the world since the 1970s using oceanographic vessels, the team of seven scientists were able to digitally map the fluxes of organic matter throughout the oceans. The resulting new estimate of storage capacity is 15 gigatonnes per year, an increase of around 20% on the previous studies (11 gigatonnes per year) reported by the IPCC in its 2021 report.

This reassessment of the seabed’s storage capacity represents a significant advance in our understanding of carbon exchanges between the atmosphere and the ocean at a global level. While the team stresses that this absorption process takes place over tens of thousands of years, and is therefore not sufficient to offset the exponential increase in CO2 emissions generated by global industrial activity since 1750, this study nevertheless reinforces the importance of the ocean ecosystem as a major player in regulating the global climate in the long term.

Global distribution of organic carbon flux from the surface layer of the open ocean.
© Wang et al., 2023, Nature.

 

Reference:

Biological carbon pump estimate based on multi-decadal hydrographic data. Wei-Lei Wang, Weiwei Fu, Frédéric A. C. Le Moigne, Robert T. Letscher, Yi Liu, Jin-Ming Tang, and François W. Primeau. Nature, le 6 décembre 2023.
DOI : https://doi.org/10.1038/s41586-023-06772-4

/by

Copyright : Laboratoire LEMAR- 2018

Login

Intranet

IUEM intranet

Directory

Contact

Legal notice

Privacy policy