Filling the gap: A 60 ky record of mixed carbonate-siliciclastic turbidite deposition from the Great Barrier Reef

Late Pleistocene to Holocene margin sedimentation on the Great Barrier Reef, a mixed carbonate-siliciclastic margin, has been explained by a transgressive shedding model. This model has challenged widely accepted sequence stratigraphic models in terms of the timing and type of sediment (i.e. carbonate vs. siliciclastic) deposited during sea-level oscillations. However, this model documents only hemipelagic sedimentation and the contribution of coarse-grained turbidite deposition, and the role of submarine canyons in this process, remain elusive on this archetypal margin. Here we present a new model of turbidite deposition for the last 60 ky in the north-eastern Australia margin. Using high-resolution bathymetry, 58 new and existing radiometric ages, and the composition of 81 turbidites from 15 piston cores, we found that the spatial and temporal variation of turbidites is controlled by the relationship between sea-level change and the variable physiography along the margin. Siliciclastic and mixed carbonate-siliciclastic turbidites were linked to canyons indenting the shelf-break and the well-developed shelf-edge reef barriers that stored sediment behind them. Turbidite deposition was sustained while the sea-level position allowed the connection and sediment bypassing through the inter-reef passages and canyons. Carbonate turbidites dominated in regions with more open conditions at the outer-shelf and where slope-confined canyons dominated or where canyons are generally less abundant. The turn-on and maintenance of carbonate production during sea-level fluctuations also influenced the timing of carbonate turbidite deposition. We show that a fundamental understanding of the variable physiography inherent to mixed carbonate-siliciclastic margins is essential to accurately interpret deep-water, coarse-grained deposition within a sequence stratigraphic context.     

Street hierarchies: a minority of streets account for a majority of traffic flow

Urban streets are hierarchically organized in the sense that a majority of streets are trivial, while a minority of streets is vital. This hierarchy can be simply, but elegantly, characterized by the 80/20 principle, i.e. 80% of streets are less connected (below the average), while 20% of streets are well connected (above the average); out of the 20%, there is 1% of streets that are extremely well connected. This paper, using a European city as an example, examined, at a much more detailed level, such street hierarchies from the perspective of geometric and topological properties. Based on an empirical study, we further proved a previous conjecture that a minority of streets accounts for a majority of traffic flow; more accurately, the 20% of top streets accommodate 80% of traffic flow (20/80), and the 1% of top streets account for more than 20% of traffic flow (1/20). Our study provides new evidence as to how a city is (self‐)organized, contributing to the understanding of cities and their evolution using increasingly available mobility geographic information.     

A human-machine adversarial scoring framework for urban perception assessment using street-view images

ABSTRACT

Though global-coverage urban perception datasets have been recently created using machine learning, their efficacy in accurately assessing local urban perceptions for other countries and regions remains a problem. Here we describe a human-machine adversarial scoring framework using a methodology that incorporates deep learning and iterative feedback with recommendation scores, which allows for the rapid and cost-effective assessment of the local urban perceptions for Chinese cities. Using the state-of-the-art Fully Convolutional Network (FCN) and Random Forest (RF) algorithms, the proposed method provides perception estimations with errors less than 10%. The driving factor analysis from both the visual and urban functional aspects demonstrated its feasibility in facilitating local urban perception derivations. With high-throughput and high-accuracy scorings, the proposed human-machine adversarial framework offers an affordable and rapid solution for urban planners and researchers to conduct local urban perception assessments.     

Flow in a Street Canyon for any External Wind Direction

An analytical model has been developed for the flow along a street canyon (of height H and width W), generated by an external wind blowing at any angle relative to the axis of the street. Initially, we consider the special case of a wind blowing parallel to the street. The interior of the street is decomposed into three regions, and the flow within each region is assumed to depend only on the external wind and the distance to the closest solid boundary. This decomposition leads to two different flow regimes: one for narrow streets (H/W > 1/2) and one for wide streets (H/W < 1/2). The theoretical model agrees well with results obtained from numerical simulations using a Reynolds-Averaged Navier–Stokes model. We then generalize the model to the case of arbitrary wind direction. Numerical solutions show that the streamlines of the mean flow in the street have a spiral form, and for most angles of incidence, the mass flux along the street scales on the component of the external wind resolved parallel to the street. We use this result to generalize the model derived for wind blowing parallel to the street, and the results from this model agree well with the numerical simulations. The model that has been developed can be evaluated rapidly using only very modest computing power, so it is suitable for use as an operational tool.     

Fine-scale relief related to Late Holocene channel shifting within the floor of the upper Redondo Fan, offshore Southern California

Erosional and depositional bedforms have been imaged at outcrop scale in the upper Redondo Fan, in the San Pedro Basin of offshore Southern California in ≥600 m water depths, using an Autonomous Underwater Vehicle developed by the Monterey Bay Aquarium Research Institute. The Autonomous Underwater Vehicle is equipped with multibeam and chirp sub-bottom sonars. Sampling and photographic images using the Monterey Bay Aquarium Research Institute Remotely Operated Vehicle Tiburon provide groundtruth for the Autonomous Underwater Vehicle survey. The 0·3 m vertical and 1·5 m lateral bathymetric resolution and 0·1 m sub-bottom profile resolution provide unprecedented detail of bedform morphology and structure. Multiple channels within the Redondo Fan have been active at different times during the Late Holocene (0 to 3000 yr bp ). The currently active channel extending from Redondo Canyon makes an abrupt 90° turn at the canyon mouth before resuming a south-easterly course along the east side of the Redondo Fan. This channel is floored by sand and characterized by small steps generally <1 m in relief, spaced 10 to 80 m in the down-channel direction. A broader channel complex lies along the western side of the fan valley that was last active more than 850 years ago. Two distinct trains of large scours, with widths ranging from tens to a few hundred metres and depths of 20 m, occur on the floor of the western channel complex, which has a thin mud drape. If observed in cross-section only, these large scours would probably be misidentified as the thalweg of an active channel.     

Influence of Building Areal Density and Roof Shape on the Wind Characteristics Above a Town

Flow characteristics in the lower part of theatmospheric boundary layer developing immediatelyabove building roofs have been studied by physicalmodelling under neutral stratification conditions. Thevertical profiles of velocity, turbulence intensityand Reynolds stress were measured in detail above amodel urban fetch consisting of parallel streetcanyons. Two different street densities and roofshapes were tested. It is found that the influence ofthe buildings on the oncoming wind remains confined towithin three overall building heights above ground.Furthermore, the effect on the wind at roof levelfrom the areal building density is relatively weak, butstrong from the roof shape. Thus, altering roof shapecan have a much more beneficial impact on urban airquality than increasing the spacing betweenbuildings. Moreover, these findings yield a novelmethodology for reliable prediction of urban airquality, by combining numerical mesoscale wind flowmodels with physical street canyon pollutiondispersion models.     

Interface bureaucrats and the everyday remaking of climate interventions: Evidence from climate change adaptation in Zambia

When climate change policies are implemented in practice, they travel through the hands of a range of practitioners who not only mediate but also potentially transform climate interventions. This article highlights the role of a group of actors whose practices have so far received little attention in the study of climate change governance, namely the public servants who are responsible for the everyday implementation of national climate change policies and associated programmes on the ground. Situated at the frontline of the state and often engaging directly with citizens, these “interface bureaucrats” occupy a complex position in which they must balance their role as representatives of the state with the need to accommodate the pressures, interests and practical challenges associated with everyday policy implementation. In this article we examine how interface bureaucrats in Zambia seek to navigate this role as they go about implementing national climate change adaptation policies in practice, and what this means for the nature and outcome of these interventions. We identify key dilemmas of the interface bureaucrats in our study areas, namely (i) intervening with limited reach, (ii) implementing generic policies, and (iii) managing conflicting interests. We show how they address these dilemmas through highly pragmatic practices involving informal agreements with community members, discretionary adjustments of official policies, and negotiation of contested interventions. As a result, the nature and outcomes of climate change adaptation interventions end up differently from the official policies and the underlying governance interests of the central state. Our findings suggest a need for greater attention to the role of interface bureaucrats as everyday climate policy makers and point to the significance of pragmatism and compromise in the interaction between state actors and citizens in environmental interventions.     

Bridging equity? Washington,D.C.’s new elevated park as a test case for just planning

In the last decade, justice has been revived as a primary criterion for the analysis and evaluation of planning policies. This paper continues this line of research by examining a proposed redevelopment project in Washington, D.C. that sets equitable development as its goal . The proposed 11th Street Bridge Park would be a top-notch elevated park, physically and symbolically connecting D.C’s wealthy west with the disadvantaged east. The project is managed by a nonprofit organization and seemingly stands out in its progressive vision: An Equitable Development Plan has been developed in an attempt to secure the future of the local residents in light of the neighborhood's anticipated gentrification. However, preliminary findings show that despite explicit commitment to equity, the planning of the park also resurfaces racial and class tensions . The analysis of procedural and substantive aspects of justice in this case suggests that issues of recognition, power and representation are instrumental to fully understand urban (in)justices.     

边界管控中的跨境社会建构:深圳中英街的案例

在社会建构视角下,边界并非固化的界线,各种社会力量亦在持续塑造着边界的功能与特性。采用深度访谈、实地调查和文本分析研究方法,从社会建构的视角,探讨了不同主体基于日常跨境实践对中英街边界的社会建构,以及在此基础上的边境空间管控应对策略。结果发现,在20世纪80年代改革开放背景下,中英街的边贸旅游经济发展为居民参与跨境小额贸易提供了契机,中英街居民的身份与水客的身份由此实现了高度的融合;而在20世纪90年代内地实行市场经济及香港回归的背景下,中英街边贸旅游经济衰落,中英街地区居民的身份与水客的身份逐渐分离。在此过程中,各主体响应边界管控政策变化,塑造了不同的边界生活空间。未来边界管控政策的制定与实施,需要以理解边界空间的历史和现状为前提。     

Geology and thermochronometry of the east edge of the Median Batholith (Median Tectonic Zone): a new perspective on Permian to Cretaceous crustal growth of New Zealand

Abstract We report new field, petrological and isotopic data and interpretations from one of New Zealand’s major basement geological boundaries, the contact between the east side of the Median Batholith (formerly Median Tectonic Zone) and the allochthonous Mesozoic terranes of the Eastern Province. In the Nelson and Hollyford–Eglinton areas this contact is a Cenozoic fault, the Median Tectonic Line of earlier workers. However, in the Longwood Range, unfaulted pre-Cenozoic geological relations are preserved intact. Our new Ar–Ar, U–Pb and isotopic data show that the Median Batholith in the Longwood Range consists of two suites. (i) Eastern, isotopically primitive (⁸⁷Sr/⁸⁶Sr_i = 0.702 to 0.703; ?_NdT = + 7 to + 8) trondhjemite and gabbroic rocks of Permian age that we believe are part of the intraoceanic Brook Street arc of the Eastern Province. (ii) Western, isotopically more evolved (⁸⁷Sr/⁸⁶Sr_i = 0.703 to 0.704; ?_NdT = + 3 to + 5) quartz diorites, quartz monzodiorites and rare granites of Middle Triassic to Early Jurassic age that we correlate with a pulse of magmatism elsewhere in the Median Batholith. Field observations in the Longwood Range indicate intrusive, not faulted, contacts between these units and constrain accretion of the Brook Street Terrane to Gondwana to have occurred 230–245 Ma. Intra-batholith shear zones (T ~ 600°C and P ~ 0.2–0.3 GPa) were active at approximately 220 Ma. Modelling of K-feldspar Ar incremental heating ages indicate that most of the Longwood Range had cooled below 175°C by the Middle Jurassic and experienced no subsequent reheating. Significant additional post-accretionary Early Cretaceous and Cenozoic thermotectonic activity in Median Batholith in the Hollyford-Eglinton area is indicated by a new 140 ± 2 Ma U-Pb zircon date on a Largs ignimbrite, as well as by Cenozoic K-feldspar Ar–Ar ages in the Middle Triassic Mistake Diorite.