Evolution diagénétique dans la craie pélagique dolomitisée du crétacé supérieur du bassin de Paris (région de Provins, France)     

Jean-Pierre Gély  Philippe Blanc 《Eclogae Geologicae Helvetiae》2004,97(3):393-409

Two deep scientific boreholes, named Poigny 701 and Sainte-Colombe 702, located in the Paris Basin near Provins (Seine-et-Marne, France), recovered a complete Upper Cretaceous chalk succession. A correlation between the boreholes lithostratigraphy, reflexion seismic profiles and diagenetic patterns shows that major velocity variations measured in the seismic reflection profiles correspond to dolomitized chalk intervals. Dolomitisations occurred during early and burial diagenesis. The understanding of these complex diagenetic events has an important economic consequence on the static correction of the chalk formation in the Paris Basin. Optimisation of petroleum prospecting below chalk cover is thus possible. The chalk series of the 701 and 702 boreholes range from the Cenomanian to the upper Campanian. In this succession, micrite has a primarily biogenic origin; it consists of pelagic organisms, indicative of warm seawater with values around 25°C. Several hiatuses occur in the 701 borehole. These hiatuses indicate the existence of particular hydrodynamic conditions. Deep-water channels were locally recognised in the Paris Basin as in Normandy and Picardy. In the 702 borehole, massive dolomitisation affected the upper meters of sediment below the sea floor. This early phase of massive dolomitisation was induced by slow circulation of a magnesium-rich seawater mass, along the seawater/sediment interface. Thus, this area was a zone of intense marine circulation between the North-West infralittoral and the South-West bathyal domains, across the London-Paris Basin. Magnesium-rich seawater had as origin the recrystallisation of the biogenic peri-plateform carbonates. During both dolomitisation and dissolution of the calcite matrix of the massive dolomite, the calcite had cemented chalk around the massive dolomite body. After deposition, the chalk series was progressively compacted and lithified by burial calcite cement. During the late Campanian-Maastrichtian, the burial compaction of the chalk and thermal gradient reached their maximum, as compressive stresses from the Pyrenean orogenesis affected the Paris Basin. At this time, compaction of the massive dolomite induced the expulsion of magnesian-rich fluids into the underlying already compacted chalk series. In 702 borehole, a diffuse dolomitisation then affected strongly underlying the chalk series. In 701 borehole, this diffuse dolomitisation affected slightly the lower half of the chalk series. Laterally, dolomitisation decreases gradually and affected a only smaller thickness of the chalk series, disappearing laterally. During the progressive emergence of the Paris Basin, from the Paleogene to the Quaternary, the chalk series were partially invaded by continental fresh water. Thus partial dedolomitisation affected the massive dolomite, whereas total dedolomitisation affected only the upper first meters of it.Manuscrit reçu le 20 juin 2003 Révision acceptée le 9 septembre 2004  相似文献   

What is the difference between two maps? A remote senser’s view     

Giles M. Foody 《Journal of Geographical Systems》2006,8(2):119-130

In remote sensing, thematic map comparison is often undertaken on a per-pixel basis and based upon measures of classification agreement. Here, the degree of agreement between two thematic maps, and so the difference between the pair, was evaluated through visual and quantitative analyses for two scenarios. Quantitative assessments were based on basic site-specific measures of agreement that are used widely in accuracy assessment (e.g. the overall percentage of pixels with the same class label in each of the two maps and the kappa coefficient of agreement) as well as an information theory based approach that allows the degree of mutual or shared information to be assessed even if different classification schemes have been used to produce the maps. The results indicated that in the first map comparison scenario, focused on labelling, there was a fair degree of correspondence between the maps but with an overall difference in information content of ∼42%. In the second comparison scenario, focused on change in time, considerable change had occurred with a change in class label for ∼42% of the pixels. It was also apparent that global assessments masked local scale changes.  相似文献   

Estimation de la température maximale d'enfouissement du Toarcien et du Callovo-Oxfordien au centre du bassin de Paris par les marqueurs organiques     

Cédric Ménétrier  Marcel Élie  Luis Martinez  Antoine Le Solleuz  Jean-Robert Disnar  Cécile Robin  François Guillocheau  Christophe Rigollet 《Comptes Rendus Geoscience》2005,337(15):1323-1330

The thermal history of the central part of the Paris basin is reconstructed using C₃₁ hopane $\mathrm{S}/\mathrm{R}$ isomerisation ratios and organic matter transformation ratios measured on Lower Toarcian and Callovo-Oxfordian samples. Maximum burial palaeotemperatures range between 90 and 115?°C for the Toarcian shales, and between 75 and 95?°C for the Callovo-Oxfordian samples, from the East to the centre of the basin, respectively. The amount of Late Cretaceous erosion was evaluated to be between ca. 400 to 600 m in the eastern part of the studied area and 100 to 300 m in the centre of the basin. To cite this article: C. Ménétrier et al., C. R. Geoscience 337 (2005).  相似文献   

Relative Influence of Urban And Orographic Effects for Low Wind Conditions in the Paris Area   总被引：1，自引：0，他引：1  

F. Troude  E. Dupont  B. Carissimo  A. I. Flossmann 《Boundary-Layer Meteorology》2002,103(3):493-505

The relative roles of land-use and orography on the meteorological fields in the Paris area are studied by means of numerical simulations of two Special Observing Periods (SOP), of the ECLAP experiment. Sensitivity experiments have been performed with flat orography to investigate the strength of the urban effects, and with a uniform land-use surface to replace the surface heterogeneities, to isolate the orographic forcing. Comparisons of the simulated fields with a reference simulation including all forcing are analysed. It is found that during these two SOP of spring-time conditions, despite the low terrain elevation, the orographic effect is the main forcing of the dynamic field but that although the land use is the dominant factor reproducing the thermal evolution of the boundary layer, the orography alone also plays a role in the temperature pattern with slope flows in and out of the Paris basin.  相似文献   

Assessing synergies and trade-offs of diverging Paris-compliant mitigation strategies with long-term SDG objectives     

《Global Environmental Change》2023

The Sustainable Development Goals (SDGs) and the Paris Agreement are the two transformative agendas, which set the benchmarks for nations to address urgent social, economic and environmental challenges. Aside from setting long-term goals, the pathways followed by nations will involve a series of synergies and trade-offs both between and within these agendas. Since it will not be possible to optimise across the 17 SDGs while simultaneously transitioning to low-carbon societies, it will be necessary to implement policies to address the most critical aspects of the agendas and understand the implications for the other dimensions. Here, we rely on a modelling exercise to analyse the long-term implications of a variety of Paris-compliant mitigation strategies suggested in the recent scientific literature on multiple dimensions of the SDG Agenda. The strategies included rely on technological solutions such as renewable energy deployment or carbon capture and storage, nature-based solutions such as afforestation and behavioural changes in the demand side. Results for a selection of energy-environment SDGs suggest that some mitigation pathways could have negative implications on food and water prices, forest cover and increase pressure on water resources depending on the strategy followed, while renewable energy shares, household energy costs, ambient air pollution and yield impacts could be improved simultaneously while reducing greenhouse gas emissions. Overall, results indicate that promoting changes in the demand side could be beneficial to limit potential trade-offs.  相似文献   

The effectiveness of climate clubs under Donald Trump     

Detlef F. Sprinz  Håkon Sælen  Arild Underdal  Jon Hovi 《Climate Policy》2018,18(7):828-838

On 1 June 2017, President Trump announced that the US intends to leave the Paris Agreement if no alternative terms acceptable to his administration can be agreed upon. In this article, an agent-based model of bottom-up climate mitigation clubs is used to derive the impact that lack of US participation may have on the membership of such clubs and their emissions coverage. We systematically analyse the prospects for climate mitigation clubs, depending on which of three conceivable roles the US takes on: as a leader (for benchmarking), as a follower (i.e. willing to join climate mitigation clubs initiated by others if this is in its best interest) or as an outsider (i.e. staying outside of any climate mitigation club no matter what). We investigate these prospects for three types of incentives for becoming a member: club goods, conditional commitments and side-payments. Our results show that lack of US leadership significantly constrains climate clubs’ potential. Lack of US willingness to follow others’ lead is an additional, but smaller constraint. Only in a few cases will US withdrawal entail widespread departures by other countries. We conclude that climate mitigation clubs can function without the participation of an important GHG emitter, given that other major emitters show leadership, although these clubs will rarely cover more than 50% of global emissions.

Key policy insights

• The US switching from being a leader to being a follower substantially reduces the emissions coverage of climate mitigation clubs.

• The US switching from being a follower to being an outsider sometimes reduces coverage further, but has a smaller impact than the switch from leader to follower.

• The switch from follower to outsider only occasionally results in widespread departures by other countries; in a few instances it even entices others to join.

• Climate mitigation clubs can function even without the participation of the US, provided that other major emitters show leadership; however, such clubs will typically be unable to cover more than 50% of global emissions.

• Climate mitigation clubs may complement the Paris Agreement and can also serve as an alternative in case Paris fails.

  相似文献   

巴黎协定背景下全球减排博弈模拟研究     

吴静  朱潜挺  王诗琪  王铮 《气候变化研究进展》2018,14(2):182-190

构建了具有7个国家集团的全球多国家集团气候博弈集成评估模拟系统,针对《巴黎协定》背景下各国至2050年以及2100年的减排目标,分别对减排博弈的纳什均衡、博弈不确定性以及外部政策对减排博弈的影响展开了模拟分析。研究发现：在基准情景下,全球各国将在2030年后均选择不减排策略,全球至2100年升温达到2.62℃;而模型参数的不确定性也未能突破全球零减排的纳什均衡;而仅当在全球范围内对不减排采取惩罚措施时,全球零减排的纳什均衡点被打破。但在当前《巴黎协定》减排承诺下,为达到2℃的温控目标,加大2030—2050年的减排幅度至关重要,否则全球将在2040年左右突破2℃阈值。  相似文献   

《巴黎协定》特设工作组适应信息通报谈判的最新进展和展望     

陈敏鹏  张宇丞  刘硕  李玉娥 《气候变化研究进展》2018,14(2):191-200

适应信息通报作为《巴黎协定》下联结国家个体适应行动、全球适应目标以及全球集体适应努力的纽带,是目前《巴黎协定》特设工作组（APA）下唯一的适应议题,会对未来全球适应气候变化的政策和行动产生较大影响。本文总结了APA适应信息通报的谈判进程和最新进展,梳理了不同缔约方和谈判集团对适应信息通报目的、内容、报告渠道、指南和灵活性的立场和观点,展望了适应信息通报未来的谈判走势。中国与大多数发展中国家相比,开展适应行动及提供信息报告的能力较强,在适应信息通报谈判中立场相对灵活,但未来在有关适应的资金支持谈判等方面仍面临着压力,建议推动和深化适应气候变化领域南南合作以团结更多发展中国家,促进全球适应行动,回应发展中国家的关切。  相似文献   

走向《巴黎协定》温升目标：已经在路上     

姜克隽  冯升波 《气候变化研究进展》2021,17(1):1-6

目前欧盟、中国、日本、韩国、加拿大,以及南非等国家或地区,已经公布了温室气体中和或者碳中和的目标,如果加上很可能很快也会提出碳中和目标的美国,全球有可能近70%的CO₂排放的国家或地区提出碳中和的目标。由于这些国家或地区是全球技术主导和经济主导地,因而全球2050年左右实现碳中和具有可行性。2050年左右实现碳中和,即和《巴黎协定》2℃目标,甚至和其1.5℃温升目标下的减排路径相一致。研究表明实现2050年左右碳中和有其可行性,实现该目标需要更多的技术创新,未来将是各个国家技术竞争和经济竞争阶段。  相似文献   

Informing national adaptation for sustainable development through spatial systems modelling     

《Global Environmental Change》2021

Acute climate-change hazards, such as floods or storm surges, can affect a nation’s built and natural environment assets that are critical for development and achievement of the Sustainable Development Goals (SDGs). To reduce the impacts of such acute climate-change hazards and safeguard development, national decision-makers require evidence on where and how hazards affect SDG achievement to better inform adaptation. Here, we develop a systems methodology that spatially models the impacts of climate-change hazards across a nation’s entire built and natural environment assets and its interdependent influences on the SDG targets to inform national adaptation. We apply our methodology in Saint Lucia through a participatory approach with decision-makers across 18 government ministries, academia, and the private sector. Results reveal that acute climate-change hazards can affect half of Saint Lucia’s assets across 22 sectors, which can influence 89% of all SDG targets. Application of our methodology provided evidence on where and how to prioritise adaptation, thereby helping to add spatial granularity to 52 measures under Saint Lucia’s National Adaptation Plan (NAP) as well as specificity on how limited capacity for cross-sectoral coordination can be directed to safeguard SDG targets. Adaptation does not necessarily imply investing in physical asset protection: results show the need to protect critical natural environments which provide important adaptation services to the built environment. As more nations develop and revise their NAPs and Nationally Determined Contributions under the Paris Agreement, strategic planning across sectors – as demonstrated in Saint Lucia – will be critical to facilitate adaptation that safeguards SDG achievement.  相似文献