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linking the Gawler Craton and Mount Isa Province through hydrothermal systems in the Peake and Denison Domain,northeastern Gawler Craton

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Geoscience Frontiers 2023年第5期14卷 108-125页

作者： Mitchell J.Bockmann justin l.payne Martin Hand laura J.Morrissey Antonio P.Belperio Department of Earth Sciences University of AdelaideAdelaideSAAustralia Mineral Exploration Cooperative Research Centre University of AdelaideAdelaideSAAustralia UniSA STEM University of South AustraliaAdelaideSAAustralia Mineral Exploration Cooperative Research Centre Future Industries InstituteUniversity of South AustraliaAdelaideSAAustralia Demetallica ltd NorwoodSAAustralia

Tectonic reconstructions of Proterozoic Australia commonly place the Peake and Denison Domain of the northeastern Gawler Craton at the interface between the North and South Australian cratons prior to the reconfiguration of Australia’s main tectonic components in the ***,this reconstruction is largely based on palaeomagnetic data as the geological correlations between these regions are currently limited,particularly during the *** early Mesoproterozoic period is significant as it corresponds to major IOCG mineralization in the eastern Gawler Craton between 1600 Ma and 1575 Ma,and IOCG mineralization in the Mount Isa Province largely between 1550 Ma and 1490 ***,determining the relationship of the Peake and Denison Domain to the Gawler Craton and Mount Isa Province during this period is essential to evaluating mineral prospectivity in the northeastern Gawler *** U–Pb lA-ICP-MS geochronology on zircon and titanite improves our understanding of the tectonothermal and hydrothermal history the Peake and Denison Domain during the latePalaeoproterozoic,early-Mesoproterozoic and the Cambrian–Ordovician *** formed within largely calc-silicate alteration assemblages indicates the Peake and Denison Domain has a protracted history of hydrothermal activity,recording events at c.1565 Ma,1530–1515 Ma,c.1500 Ma,c.1465 Ma and c.490 *** highly calcic nature of the c.1565–1500 Ma alteration in the Peake and Denison Domain shares strong similarities in age and character to the regional calcic-sodic alteration recorded in the Mount Isa *** suggest the two regions were influenced by similar hydrothermal systems during the early Mesoproterozoic,supporting reconstruction models that place the Peake and Denison Domain near the Mount Isa Province during the *** highlights the prospectivity of the Peake and Denison Domain for Isan-style IOCG mineralization,but requires consideration of the post-

关键词： Peake and Denison Gawler Craton Mount Isa IOCG Tectonic reconstruction Titanite

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Tracking the Cretaceous transcontinental Ceduna River through Australia:The hafnium isotope record of detrital zircons from offshore southern Australia

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Geoscience Frontiers 2016年第2期7卷 237-244页

作者： Jarred lloyd Alan S.Collins justin l.payne Stijn Glorie Simon Holford Anthony J.Reid Centre for Tectonics Resources and Exploration(TRaX)Department of Earth SciencesThe University of Adelaide Centre for Tectonics Resources and Exploration(TRaX)School of Built and Natural EnvironmentsThe University of South Australia Centre for Tectonics Resources and Exploration(TRaX)Australian School of PetroleumThe University of Adelaide Geological Survey of South Australia Department of State DevelopmentGovernment of South Australia

The middle-upper Cretaceous Ceduna River system traversed continental Australia from the NE coast to the centre of the southern coast. At its mouth, it formed a vast delta system that is similar in scale to the Niger delta of West Africa. The delta system is composed of two main lobes that represent different phases of delta construction. A recent hypothesis has challenged the traditional idea that both lobes of the delta were derived from a transcontinental river system by suggesting that the upper lobe （Santonian -Maastrichtian） is instead derived from a restricted catchment within southern Australia. Hf isotopic data presented here fingerprint the original source of the upper delta lobe zircons to NE Australia, with data comparing well with similar U-Pb and lu-Hf isotopic data from the lachlan Orogen, the New England Orogen, the eastern Musgraves Province and the northern Flinders Ranges. These data do not preclude a model where the lobe is derived from recycled Eromanga Basin sediments during a phase of late Cretaceous inland Australian uplift, but when coupled with reconnaissance low-temperature thermochronometry from the region of the Ceduna River course indicating widespread Triassic-Jurassic exhumation, and comparisons with detrital zircon data from the Winton Formation upstream of any proposed uplift, we suggest that both lobes of the Ceduna Delta are likely to be derived from a transcontinental Ceduna River.

关键词： Detrital zircon Hf U-Pb Ceduna sub-basin Bight basin Australia

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Magmatism and metamorphism at ca. 1.45 Ga in the northern Gawler Craton: The Australian record of rifting within Nuna(Columbia)

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Geoscience Frontiers 2019年第1期10卷 175-194页

作者： laura J.Morrissey Karin M.Barovich Martin Hand Katherine E.Howard justin l.payne School of Natural and Built Environments University of South Australia Department of Earth Sciences School of Physical Sciences University of Adelaide

U-Pb monazite and zircon geochronology and calculated metamorphic phase diagrams from drill holes in the northern Gawler Craton, southern Australia, reveal the presence of ca. 1.45 Ga magmatism and metamorphism. Magmatism and granulite facies metamorphism of this age has not previously been recognised in the Gawler Craton. The magmatic rocks have steep lREE-enriched patterns and high Ga/Al values, suggesting they are A-type granites. Calculated metamorphic forward models suggest that this event was associated with high apparent thermal gradients and reached pressures of 3.2 -5.4 kbar and temperatures of 775-815℃. The high apparent thermal gradients may reflect pluton-enhanced metamorphism, consistent with the presence of A-type granites. The recognition of ca. 1.45 Ga tectonism in the northern Gawler Craton is added to a compilation of ca. 1.50 -1.40 Ga magmatism, shear zone reactivation, rift basin development and isotope resetting throughout the South and North Australian Cratons that shows that this event was widespread in eastern Proterozoic Australia. This event is stylistically similar to ca. 1.45 Ga A-type magmatism and high thermal gradient metamorphism in laurentia in this interval and provides further support for a connection between Australia and laurentia during the Mesoproterozoic. The tectonic setting of the 1.50-1.40 Ga event is unclear but may record rifting within the Nuna(or Columbia) supercontinent, or a period of intracontinental extension within a long-lived convergent setting.

关键词： Gawler Craton laurentia Metamorphism U-Pb geochronology Paleogeographic reconstruction

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late syn-to post-collisional magmatism in Madagascar:The genesis of the Ambalavao and Maevarano Suites

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Geoscience Frontiers 2019年第6期10卷 2063-2084页

作者： Donnelly B.Archibald Alan S.Collins John D.Foden justin l.payne Peter Holden Théodore Razakamanana Department of Earth Sciences St.Francis Xavier UniversityPhysical Sciences Complex5009 Chapel SquareAntigonishNSB2G 2W5Canada Centre for Tectonics Resources and Exploration(TRaX)Department of Earth SciencesThe University of AdelaideAdelaide 5005SAAustralia Centre for Tectonics Resources and Exploration(TRaX)School of Built and Natural EnvironmentsUniversity of South AustraliaMawson LakesSA5001Australia Research School of Earth Sciences The Australian National UniversityCanberraACT2601Australia Departement des Sciences de la Terre Universitede ToliaraToliara601Madagascar

The East African Orogen involves a collage of Proterozoic microcontinents and arc terranes that became wedged between older cratonic blocks during the assembly of *** Ediacaran-Cambrian Ambalavao and Maevarano Suites in Madagascar were emplaced during the waning orogenic stages and consist of weakly deformed to undeformed plutonic rocks and dykes of mainly porphyritic granite but also gabbro,diorite and charnockite.U-Pb geochronological data date emplacement of the Ambalavao Suite to between ca.580 Ma and 540 Ma and the Maevarano Suite to between ca.537 Ma and522 *** and trace element concentrations are consistent with emplacement in a syn-to postcollisional tectonic setting as A-type(anorogenic) ***(δ^(18)O of 5.27‰-7.45‰) and hafnium(ε(Hf)(t) of-27.8 to-12.3) isotopic data from plutons in the Itremo and Antananarivo Domains are consistent with incorporation of an ancient crustal *** primitive δ^(18)O(5.27‰-5.32‰) andε(Hf)(t)(+0.0 to+0.2) isotopic values recorded in samples collected from the Ikalamavony Domain demonstrate the isotopic variation of basement sources present in the Malagasy *** Hf isotopic composition of Malagasy zircon are unlike more juvenile Ediacaran-Cambrian zircon sou rces elsewhere in the East African Orogen and,as such,Madagascar represents a distinct and identifiable detrital zircon source region in Phanerozoic sedimentary provenance *** together,these data indicate that high-T crustal anatexis,crustal assimilation and interaction of crustal material with mantle-derived melts were the processes operating during magma *** magmatism was coeval with polyphase deformation throughout Madagascar during the amalgamation of Gondwana and magmatism is interpreted to reflect lithospheric delamination of an extensive orogenic plateau.

关键词： Madagascar geology East African orogen Zircon geochronology Zircon oxygen and hafnium isotopes Post-collisional magmatism

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Phanerozoic co-evolution of O2-CO2 and ocean habitability

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National Science Review 2024年第6期11卷 18-21页

作者： Zunli lu Rosalind E.M.Rickaby Jonathan l.payne Ashley N.Prow Department of Earth & Environmental Sciences Syracuse University Department of Earth Sciences University of Oxford Department of Earth and Planetary Sciences Stanford University

Atmospheric carbon dioxide and oxygen concentrations are partially linked via the geological cycle of organic carbon （Fig. 1A–C; e.g. CO2+H2O■CH2O+O2）. The history of these two biologically active components, controls on their concentrations, and implications for the complexity of the biosphere and habitability of Earth have been hotly debated, but are generally considered independently.

关键词： ocean co-evolution habitability phanerozoic

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A gap-free genome assembly of Chlamydomonas reinhardtii anddetection of translocations induced by CRISPR-mediated mutagenesis

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Plant Communications 2023年第2期4卷 249-271页

作者： Zachary l.payne Gervette M.Penny Tychele N.Turner Susan K.Dutcher Department of Genetics Washington University School of MedicineSaint LouisMO 63110USA

Genomic assemblies of the unicellular green alga Chlamydomonas reinhardtii have provided important resources for ***,assembly errors,large gaps,and unplaced scaffolds as well as strain-specific variants currently impede many types of *** combining PacBio HiFi and Oxford Nanopore long-read technologies,we generated a de novo genome assembly for strain CC-5816,derived from crosses of strains CC-125 and *** methods of evaluating genome completeness and base-pair error rate suggest that the final telomere-to-telomere assembly is highly *** CC-5816 assembly enabled previously difficult analyses that include characterization of the 17 centromeres,rDNA arrays on three chromosomes,and 56 insertions of organellar DNA into the nuclear *** Nanopore sequencing,we identified sites of cytosine(CpG)methylation,which are enriched at *** analyzed CRISPR-Cas9 insertional mutants in the PF23 *** of the three alleles produced progeny that displayed patterns of meiotic inviability that suggested the presence of a chromosomal *** Nanopore reads from pf23-2 and pf23-3 onto the CC-5816 genome showed that these two strains each carry a translocation that was initiated at the PF23 gene locus on chromosome 11 and joined with chromosomes 5 or 3,*** translocations were verified by demonstrating linkage between loci on the two translocated chromosomes in meiotic *** three pf23 alleles display the expected short-cilia phenotype,and immunoblotting showed that pf23-2 lacks the PF23 *** CC-5816 genome assembly will undoubtedly provide an important tool for the Chlamydomonas research community.

关键词： alga reference genome de novo PacBio Nanopore structural variation

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Understanding the agronomic impacts of defoliation strategies in“Bulldog 805”Alfalfa+“Tifton 85”bermudagrass mixed stands

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Grassland Research 2023年第4期2卷 251-259页

作者： lisa l.Baxter justin C.Burt Mary Kimberly Mullenix Sydney l.payne Kaylyn R.Reagin Katie M.Mason Chris G.Prevatt Jennifer J.Tucker Department of Crop and Soil Science University of GeorgiaTiftonGeorgiaUSA Department of Animal Science Auburn UniversityAuburnAlabamaUSA Department of Animal Science University of TennesseeKnoxvilleTennesseeUSA Beef Cattle and Forage Commodity Director Alabama Farmers Federation MontgomeryMontgomeryAlabamaUSA Department of Animal and Dairy Science University of GeorgiaTiftonGeorgiaUSA

Background:The incorporation of legumes,specifically alfalfa(Medicago sativa l.),into bermudagrass(Cynodon spp.)-based pasture systems in the southeastern United States has increased in recent years as an alternative to synthetic nitrogen(N)***:A small plot evaluation was conducted in Shorter,Alabama,and Tifton,Georgia,USA,to evaluate the impact of harvest height(HH)and harvest frequency(HF)on agronomic characteristics of alfalfa+bermudagrass mixtures in southeastern United ***:Results from both locations revealed that the longer the HF and the shorter the HH,the greater the alfalfa retention was in the stand(plue parameters,while longer HF resulted in lower total digestible nutrients,lower crude protein,higher acid detergent fiber,and lower 48 h in vitro dry matter digestibility(plation at both locations(plted in different trends at each location,while longer frequencies generally increased forage ***:This research confirmed recent findings from comparable evaluations in the southeastern United States,in that increasing HH and decreasing HF improved alfalfa retention while having a negligible effect on nutritive value or forage accumulation.

关键词： alfalfa+bermudagrass mixtures defoliation management forage management

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Neoproterozoic tectonic geography of the south-east Congo Craton in Zambia as deduced from the age and composition of detrital zircons

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Geoscience Frontiers 2019年第6期10卷 2045-2061页

作者： Brandon l.Alessio Alan S.Collins Peter Siegfried Stijn Glorie Bert De Waele justin payne Donnelly B.Archibald Centre for Tectonics Resources and Exploration(TRaX)Dept of Earth SciencesThe University of AdelaideAdelaideSouth Australia 5005Australia GeoAfrica Prospecting Services cc ErosNamibia SRK Consulting 1/10 Richardson StWest PerthWestern Australia 6005Australia Curtin University of Technology Kent StBentleyWestern Australia 6102Australia Centre for Tectonics Resources and Exploration(TRaX)School of Built and Natural EnvironmentsUniversity of South AustraliaAdelaideSouth Australia 5000Australia St.Francis Xavier University Physical Sciences Complex5009 Chapel SquareAntigonishNova Scotia B2G 2W5Canada

The Southern Irumide Belt(SIB)is an orogenic belt consisting of a number of lithologically varied Mesoproterozoic and Neoproterozoic terranes that were thrust upon each *** belt lies along the southwest margin of the Archaean to Proterozoic Congo Craton,and bears a Neoproterozoic tectonothermal overprint relating to the Neoproterozoic-Cambrian collision between the Congo and Kalahari *** preserves a record of about 500 million years of plate interaction along this part of the Congo *** zircon samples from the SIB were analysed for U-Pb and lu-Hf isotopes,as well as trace element *** data are used to constrain sediment-source relationships between SIB terranes and other Gondwanan terranes such as the local Congo Craton and Irumide belt and wider afield to Madagascar(Azania)and *** correlations are then used to interpret the Mesoproterozoic to Neoproterozoic affinity of the rocks and evolution of the *** zircon samples from the Chewore-Rufunsa and Kacholola(previously referred to as luangwa-Nyimba)terranes of the SIB yield zircon U-Pb age populations and evolvedε(Hf)(t)values that are similar to the Muva Supergroup found throughout eastern Zambia,primarily correlating with Ubendian-Usagaran(ca.2.05-1.80 Ga)phase magmatism and a cryptic basement terrane that has been suggested to underlie the Bangweulu Block and Irumide *** data suggest that the SIB was depositionally connected to the Congo Craton throughout the *** more eastern Nyimba-Sinda terrane of the SIB(previously referred to as Petauke-Sinda terrane)records detrital zircon ages andε(Hf)(t)values that correlate with ca.1.1-1.0 Ga magmatism exposed elsewhere in the SIB and Irumide *** ascribe this difference in age populations to the polyphase development of the province,where the sedimentary and volcanic rocks of the Nyimba-Sinda terrane accumulated in extensional basins that developed in the *** deposition wou

关键词： Detrital zircon geochronology Tectonics Hafnium isotopes Zambia Southern irumide belt Irumide belt

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Altered expression of m^(1)A regulatory genes is associated with oncogenic pathways,overall survival,and infiltration of immune cells in diverse human cancers

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Genes & Diseases 2023年第3期10卷 739-742页

作者： Renhua Song justin J-l Wong Epigenetics and RNA Biology Program Centenary Institute The University of SydneyCamperdown 2050Australia Faculty of Medicine and Health The University of SydneyCamperdown 2050Australia

Of over 170 types of RNA modifications discovered,N^(6)-methyladenosine(m^(6)A)is the most actively studied.m6A confers oncogenic potential,maintains cancer stem cells,and is associated with cancer-related outcomes.^(... 详细信息

关键词： cancer maintain immune

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Eigenvalues of Elliptic Systems for the Mixed Problem in Perturbations of lipschitz Domains with Nonhomogeneous Neumann Boundary Conditions

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Journal of Partial Differential Equations 2020年第1期33卷 48-63页

作者： MIYAZAKI Kohei TAYlOR justin l. Department of Mathematics&Statistics Murray State UniversityMurrayKentuckyU.S.A

We study eigenvalues of an elliptic operator with mixed boundary conditions on very general decompositions of the *** impose nonhomogeneous conditions on the part of the boundary where the Neumann term lies in a certain Sobolev or lp *** work compares the behavior of and gives a relationship between the eigenvalues and eigenfunctions on the unperturbed and perturbed domains,respectively.

关键词： Eigenvalues elliptic systems mixed problem perturbed domains

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