In the field: an interview with Roger Hanlon

Roger Hanlon is a Senior Scientist at the Marine Biological Laboratory, USA, where he investigates body patterning and colour change in cephalopods. After his undergraduate degree in 1969 at Florida State University, USA, he joined the US Army and travelled before completing his MSc (1975) and PhD (1978) at the University of Miami Rosenstiel School of Marine and Atmospheric Sciences, USA. After a NATO Postdoctoral Fellowship at the University of Cambridge, UK, in 1981, Hanlon joined the Marine Biomedical Institute, University of Texas Medical Branch, where he became a full Professor, before joining the Marine Biological Laboratory in 1995. Hanlon talks about the seminal experience in his early 20s that inspired his career and the methods and equipment he uses to study cephalopod camouflage and communication across the globe.

Unity or Fragmentation in the Deep Blue: Choices in Institutional Design for Marine Biological Diversity in Areas Beyond National Jurisdiction

Delegations are in the final stages of negotiating the proposed Agreement under the United Nations Convention on the Law of the Sea on the conservation and sustainable use of marine biological diversity of areas beyond national jurisdiction (BBNJ Agreement or Agreement). The Agreement will have tremendous scope. Geographically it covers all ocean areas beyond national jurisdiction, meaning approximately 60 percent of the earth’s surface. Substantively it deals with a range of complex topics necessary for the conservation and sustainable use of marine biological diversity of areas beyond national jurisdiction, including marine genetic resources, sharing of benefits, measures such as area-based management tools, including marine protected areas, environmental impact assessments and capacity-building and the transfer of marine technology. Existing scholarship primarily explores the substantive choices for the Agreement; little examines its proposed institutional structure. This article critically assesses the competing positions advanced during negotiations for the Agreement’s institutional structure – the ‘global’ and ‘regional’ positions – and reviews the middle, or ‘compromise’ position adopted by the draft text. It suggests that both global and regional actors will be necessary to conserve and sustainably use marine biological diversity of areas beyond national jurisdiction, and that some form of coordinating mechanism is required to allocate responsibility for particular tasks. Two principles are proposed for use in combination to provide a mechanism to help coordinate Agreement organs (global) and regional or sectoral bodies, namely, the principles of subsidiarity and cooperation. These principles are found in existing international and regional structures but are advanced here in dynamic forms, allowing for temporary or quasi-permanent allocation of competences, which can change or evolve over time. This position is also grounded in the international law of treaties and furthers dynamic views of regional and global ocean governance by offering practical coordinating principles that work with the existing Agreement text.

Spatiotemporal variations of the δ(O₂/N₂), CO₂ and δ(APO) in the troposphere over the Western North Pacific

We analyzed air samples collected onboard a cargo aircraft C-130 over the western North Pacific from May 2012 to March 2020 for atmospheric δ(O2/N2) and CO2 amount fraction. We corrected for significant artificial fractionation of O2 and N2 caused by thermal diffusion during the air sample collection by using the simultaneously-measured δ(Ar/N2). The observed seasonal cycles of the δ(O2/N2) and atmospheric potential oxygen (δ(APO)) varied nearly in opposite phase to that of the CO2 amount fraction at all latitudes and altitudes. Seasonal amplitudes of δ(APO) decreased with latitude from 34 to 25° N, as well as with increasing altitude from the surface to 6 km by 50–70 %, while those of CO2 amount fraction decreased by less than 20 %. By comparing the observed values with the simulated δ(APO) and CO2 amount fraction values generated by an atmospheric transport model, we found that the seasonal δ(APO) cycle in the middle troposphere was modified significantly by a superposition of the northern and southern hemispheric seasonal cycles due to the inter-hemispheric mixing of air. The simulated δ(APO) underestimated the observed interannual variation in δ(APO) significantly, probably due to the interannual variation in the annual mean air-sea O2 flux. Interannual variation in δ(APO) driven by the net marine biological activities, obtained by subtracting the assumed solubility-driven component of δ(APO) from the total variation, indicated a clear evidence of influence on annual sea-to-air (air-to-sea) marine biological O2 flux during El Niño (La Niña). By analyzing the observed secular trends of δ(O2/N2) and CO2 amount fraction, global average terrestrial biospheric and oceanic CO2 uptakes for the period 2012–2019 were estimated to be (1.8 ± 0.9) and (2.8 ± 0.6) Pg a−1 (C equivalents), respectively.