Carbon Market Provisions in the Paris Agreement (Article 6). CEPS Special Report No. 128/January 2016

The markets provisions, contained in Article 6 of the Paris Agreement adopted in December 2015, can be seen as both a major success and a minor miracle. Throughout 2015, and during COP21 itself, the prediction was for a very small reference to anything related to markets, or possibly even the total omission of any such reference in the text. As predicted, the markets/non-markets text in Article 6 of the Paris Agreement (PA) was one of the last issues to be agreed, in the last night of COP21, shortly before the text went to the COP President, French Foreign Minister Laurent Fabius, for final approval and its subsequent release to the delegates for acceptance on 12 December 2015. This paper presents the evolution of the ideas contained in Article 6 of the Paris Agreement, and how these were captured in textual form in different drafts of the agreement. Understanding the origin of different provisions in the PA, and their evolution, may prove crucial. Losing the institutional memory may lead to attempts, through re-interpretation of the PA, to renegotiate it.

(Table 6a) 137Cs concentrations in waters of the Sea of Japan in 1994 and in 2002

Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along with aerobic bacteria take part in mineralization of organic matter. They exist on surfaces and in microniches of particles of organic detritus.

(Table 6b) 137Cs concentrations in surface layer bottom sediments of the Sea of Japan in 1994 and in 2002

Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along with aerobic bacteria take part in mineralization of organic matter. They exist on surfaces and in microniches of particles of organic detritus.

Chemical composition of the chalcophanite rich surface of an encrusted rock ashore Lake Macquarie, Australia

Mineralogical interest in the nature of manganese oxide particulates in natural marine water (Suess, 1979), natural lake water (Klaveness, 1977), and simulated lake water (Giovanoli, 1980), prompted a search for such particulates in a large New South Wales coastal lake. The investigated waters did show the existence of manganese oxide replacement phenomena in fragmentary sedimentary rocks near the south margin of Lake Macquarie. The black crusts of manganese oxide discovered on rocks close to the waterline have revealed a three layers structure. Layer A (0-35 micron), adjacent to the rock, is composed essentially of kaolinite of weathering origin, together with low levels of manganese oxide without detectable Zn. Layer B (35-80 micron) follows as a manganese oxide layer containing admixed kaolinite and low amounts of Zn. Layer C (80-130 micron) is the closest to the surface and is made of Chalcophanite containing 10-15% of ZnO.

(Table 2) Trace element contents in ancient Black Sea sapropelic muds

The study of vertical distribution of Mo, V, Co, Ni, and Cu in mass of Black Sea sediments showed that maximum concentrations occur in sapropelic muds of ancient Black Sea deposits. A special study of sapropels samples showed a sufficiently clear correlation of Cu, Ni, Mo, and V contents with organic carbon contents; Co contents do not show such a correlation, but show one with contents of pyrite sulfur. A study of fractions of bitumen, free humic and fulvic acids showed that some part of metal contents in the sediments is bound with organic matter. It is shown that increased concentrations of trace elements in sapropels result from removing of dissolved metals from seawater by organic detritus during deposition on the bottom, in vivo concentration of metals in plankton organisms is of secondary importance.

The works of Thomas Middleton, now first collected,

Imperfect: frontpiece wanting. cf. v.1, p. 4211.

Robert E. Lee, centennial celebration of his birth held under the auspices of the University of South Carolina on the nineteenth day of January 1907.

"Address, 'Lee, the college president, by Dr. Edward S. Joynes, formerly of General Lee's faculty": p. 19-36.

Manwood's Treatise of the forest laws : shewing not only the laws now in force, but the original of forests, what they are, and how they differ from chases, parks, and warrens; with all such things as are incident to either: together with the proper terms of art, collected out of the common and statute laws of this realm; as also from the assises and iters of Pickering and Lancaster, and several other ancient and learned authors. Treating also of the office of agistors, beadles, foresters, keepers, rangers, verderors and woodwards, and of the Courts of attachment, & c. With all the variety of cases relating to forests, chases, parks, and warrens; and all the laws concerning the game made, adjudged or repealed, since the year 1665. The whole digested under proper titles in an alphabetical order.

"Appendix. Charta de foresta, of Canvtvs, a Dane, and king of this realm; granted at a Parliament holden at Winchester, anno Dom. 1016 [and other statutes relating to forests]": p. 393-435.