Geological evolution of two crustal scale shear zones. Part I. The Rand thrust complex, northwestern Mojave Desert, California. Part II. The Magdalena metamorphic core complex, north central Sonora, Mexico

The geology and structure of two crustal scale shear zones were studied to understand the partitioning of strain within intracontinental orogenic belts. Movement histories and regional tectonic implications are deduced from observational data. The two widely separated study areas bear the imprint of intense Late Mesozoic through Middle Cenozoic tectonic activity. A regional transition from Late Cretaceous-Early Tertiary plutonism, metamorphism, and shortening strain to Middle Tertiary extension and magmatism is preserved in each area, with contrasting environments and mechanisms. Compressional phases of this tectonic history are better displayed in the Rand Mountains, whereas younger extensional structures dominate rock fabrics in the Magdalena area.

In the northwestern Mojave desert, the Rand Thrust Complex reveals a stack of four distinctive tectonic plates offset along the Garlock Fault. The lowermost plate, Rand Schist, is composed of greenschist facies metagraywacke, metachert, and metabasalt. Rand Schist is structurally overlain by Johannesburg Gneiss (= garnet-amphibolite grade orthogneisses, marbles and quartzites), which in turn is overlain by a Late Cretaceous hornblende-biotite granodiorite. Biotite granite forms the fourth and highest plate. Initial assembly of the tectonic stack involved a Late Cretaceous? south or southwest vergent overthrusting event in which Johannesburg Gneiss was imbricated and attenuated between Rand Schist and hornblende-biotite granodiorite. Thrusting postdated metamorphism and deformation of the lower two plates in separate environments. A post-kinematic stock, the Late Cretaceous Randsburg Granodiorite, intrudes deep levels of the complex and contains xenoliths of both Rand Schist and mylonitized Johannesburg? gneiss. Minimum shortening implied by the map patterns is 20 kilometers.

Some low angle faults of the Rand Thrust Complex formed or were reactivated between Late Cretaceous and Early Miocene time. South-southwest directed mylonites derived from Johannesburg Gneiss are commonly overprinted by less penetrative north-northeast vergent structures. Available kinematic information at shallower structural levels indicates that late disturbance(s) culminated in northward transport of the uppermost plate. Persistence of brittle fabrics along certain structural horizons suggests a possible association of late movement(s) with regionally known detachment faults. The four plates were juxtaposed and significant intraplate movements had ceased prior to Early Miocene emplacement of rhyolite porphyry dikes.

In the Magdalena region of north central Sonora, components of a pre-Middle Cretaceous stratigraphy are used as strain markers in tracking the evolution of a long lived orogenic belt. Important elements of the tectonic history include: (1) Compression during the Late Cretaceous and Early Tertiary, accompanied by plutonism, metamorphism, and ductile strain at depth, and thrust driven? syntectonic sedimentation at the surface. (2) Middle Tertiary transition to crustal extension, initially recorded by intrusion of leucogranites, inflation of the previously shortened middle and upper crustal section, and surface volcanism. (3) Gravity induced development of a normal sense ductile shear zone at mid crustal levels, with eventual detachment and southwestward displacement of the upper crustal stratigraphy by Early Miocene time.

Elucidation of the metamorphic core complex evolution just described was facilitated by fortuitous preservation of a unique assemblage of rocks and structures. The "type" stratigraphy utilized for regional correlation and strain analysis includes a Jurassic volcanic arc assemblage overlain by an Upper Jurassic-Lower Cretaceous quartz pebble conglomerate, in turn overlain by marine strata with fossiliferous Aptian-Albian limestones. The Jurassic strata, comprised of (a) rhyolite porphyries interstratified with quartz arenites, (b) rhyolite cobble conglomerate, and (c) intrusive granite porphyries, are known to rest on Precambrian basement north and east of the study area. The quartz pebble conglomerate is correlated with the Glance Conglomerate of southeastern Arizona and northeastern Sonora. The marine sequence represents part of an isolated arm? of the Bisbee Basin.

Crosscutting structural relationships between the pre-Middle Cretaceous supracrustal section, younger plutons, and deformational fabrics allow the tectonic sequence to be determined. Earliest phases of a Late Cretaceous-Early Tertiary orogeny are marked by emplacement of the 78 ± 3 Ma Guacomea Granodiorite (U/Pb zircon, Anderson et al., 1980) as a sill into deep levels of the layered Jurassic series. Subsequent regional metamorphism and ductile strain is recorded by a penetrative schistosity and lineation, and east-west trending folds. These fabrics are intruded by post-kinematic Early Tertiary? two mica granites. At shallower crustal levels, the orogeny is represented by north directed thrust faulting, formation of a large intermontane basin, and development of a pronounced unconformity. A second important phase of ductile strain followed Middle Tertiary? emplacement of leucogranites as sills and northwest trending dikes into intermediate levels of the deformed section (surficial volcanism was also active during this transitional period to regional extension). Gravitational instabilities resulting from crustal swelling via intrusion and thermal expansion led to development of a ductile shear zone within the stratigraphic horizon occupied by a laterally extensive leucogranite sill. With continued extension, upper crustal brittle normal faults (detachment faults) enhanced the uplift and tectonic denudation of this mylonite zone, ultimately resulting in southwestward displacement of the upper crustal stratigraphy.

Strains associated with the two ductile deformation events have been successfully partitioned through a multifaceted analysis. R_f/Ø measurements on various markers from the "type" stratigraphy allow a gradient representing cumulative strain since Middle Cretaceous time to be determined. From this gradient, noncoaxial strains accrued since emplacement of the leucogranites may be removed. Irrotational components of the postleucogranite strain are measured from quartz grain shapes in deformed granites; rotational components (shear strains) are determined from S-C fabrics and from restoration of rotated dike and vein networks. Structural observations and strain data are compatable with a deformation path of: (1) coaxial strain (pure shear?), followed by (2) injection of leucogranites as dikes (perpendicular to the minimum principle stress) and sills (parallel to the minimum principle stress), then (3) southwest directed simple shear. Modeling the late strain gradient as a simple shear zone permits a minimum displacement of 10 kilometers on the Magdalena mylonite zone/detachment fault system. Removal of the Middle Tertiary noncoaxial strains yields a residual (or pre-existing) strain gradient representative of the Late Cretaceous-Early Tertiary deformation. Several partially destrained cross sections, restored to the time of leucogranite emplacement, illustrate the idea that the upper plate of the core complex bas been detached from a region of significant topographic relief. 50% to 100% bulk extension across a 50 kilometer wide corridor is demonstrated.

Late Cenozoic tectonics of the Magdalena region are dominated by Basin and Range style faulting. Northeast and north-northwest trending high angle normal faults have interacted to extend the crust in an east-west direction. Net extension for this period is minor (10% to 15%) in comparison to the Middle Tertiary detachment related extensional episode.

Phosphorylation of synaptic vesicle proteins: modulation of the alpha SNAP interaction with the core complex.

We analyzed whether synaptic membrane trafficking proteins are substrates for casein kinase II, calcium/calmodulin-dependent protein kinase II, and cAMP-dependent protein kinase (PKA), three kinases implicated in the modulation of synaptic transmission. Each kinase phosphorylates a specific set of the vesicle proteins syntaxin 1A, N-ethylmaleimide-sensitive factor (NSF), vesicle-associated membrane protein (VAMP), synaptosome-associated 25-kDa protein (SNAP-25), n-sec1, alpha soluble NSF attachment protein (alpha SNAP), and synaptotagmin. VAMP is phosphorylated by calcium/calmodulin-dependent protein kinase II on serine 61. alpha SNAP is phosphorylated by PKA; however, the beta SNAP isoform is phosphorylated only 20% as efficiently. alpha SNAP phosphorylated by PKA binds to the core docking and fusion complex 10 times weaker than the dephosphorylated form. These studies provide a first glimpse at regulatory events that may be important in modulating neurotransmitter release during learning and memory.

CONSTRAINTS ON THE LITHOSPHERIC STRUCTURE OF MID OCEAN RIDGES FROM OCEANIC CORE COMPLEX MORPHOLOGY

The Mid-oceanic ridge system is a feature unique to Earth. It is one of the fundamental components of plate tectonics and reflects interior processes of mantle convection within the Earth. The thermal structure beneath the mid-ocean ridges has been the subject of several modeling studies. It is expected that the elastic thickness of the lithosphere is larger near the transform faults that bound mid-ocean ridge segments. Oceanic core complexes (OCCs), which are generally thought to result from long-lived fault slip and elastic flexure, have a shape that is sensitive to elastic thickness. By modeling the shape of OCCs emplaced along a ridge segment, it is possible to constraint elastic thickness and therefore the thermal structure of the plate and how it varies along-axis. This thesis builds upon previous studies that utilize thin plate flexure to reproduce the shape of OCCs. I compare OCC shape to a suite of models in which elastic thickness, fault dip, fault heave, crustal thickness, and axial infill are systematically varied. Using a grid search, I constrain the parameters that best reproduce the bathymetry and/or the slope of ten candidate OCCs identified along the 12°—15°N segment of the Mid-Atlantic Ridge. The lithospheric elastic thicknesses that explains these OCCs is thinner than previous investigators suggested and the fault planes dip more shallowly in the subsurface, although at an angle compatible with Anderson’s theory of faulting. No relationships between model parameters and an oceanic core complexes location within a segment are identified with the exception that the OCCs located less than 20km from a transform fault have slightly larger elastic thickness than OCCs in the middle of the ridge segment.

光系统I及其亚组分的分离纯化与光破坏特性的研究

光系统I（photosystem I，PSI）是光合膜上参与光合作用原初反应过程的主要膜蛋白超分子复合体之一。高等植物的PSI是由核心复合体（14个亚基）和捕光色素蛋白复合体I（light-harvesting complex I, LHCI，含4个Lhca蛋白）组成的超分子复合体，它的主要功能是调节光诱导的从囊腔侧的质体兰素（plastocyanin，PC）向基质侧的铁氧还蛋白（ferredoxin，Fd）的电子传递。研究PSI的结构与功能对于揭示植物光合作用高效吸能、传能的分子机理具有重要意义。在本文中，我们首先建立了分离制备PSI及其亚组分的方法（Qin et al., 2007），并在此基础上对PSI在强光破坏的过程中结构与功能的变化进行了比较深入的研究。本论文的主要研究结果如下： 1．快速、高效分离纯化PSI及其亚组分方法的建立。 国际上传统的PSI分离方法（Bassi and Simpson, 1987; Croce et al., 1998; Påsllon et al.1995; Schmid et al. 2002），耗时长较长（分离PSI颗粒一般需要多于20h的蔗糖超速离心过程，而分离PSI的亚组分则需要25-60h的蔗糖超速离心过程）、得率较低，这不便于PSI方面的研究，为此我们首先改进了传统的分离纯化方法。新方法以高等植物菠菜叶片作为原材料，使用Triton X-100作为增溶剂，通过差速离心技术获得的粗制品，然后使用十二烷基麦芽糖苷(n-Dodecyl β-D-maltoside, DDM)增溶PSI粗制品，之后采用100,000×g，垂直转头（Beckman VTi 50）0.1-1 mol/L蔗糖梯度离心3h获得纯度较高的PSI颗粒。然后使用DDM和3-(N, N-Dimethylpalmitylammonio) propanesulfonate （zw 3-16）两种增溶剂处理PSI，后经100,000×g，垂直转头（Beckman VTi 50）蔗糖梯度离心4h获得纯度较高的PSI core、LHCI-680、LHCI-730复合体。采用吸收光谱、荧光光谱技术研究了各样品的基本光谱学特性，采用HPLC分析了各样品的色素组成，结果显示平均每个Lhca蛋白结合1.5-1.6黄体素，1.0紫黄质, 0.8-1.1 β-胡萝卜素，该方法制备的LHCI比传统方法制备的LHCI减少了类胡萝卜素的丢失。这一工作为以后结构与功能的研究工作奠定了良好的基础。 2．PSI复合体及其亚组分的特性研究。 PSI颗粒具有一定的适应环境酸碱变化的能力，在我们的试验条件下PSI颗粒在pH 5-10相对稳定。PSI、LHCI很难通过加入Mg2+、Ca2+、Na+阳离子聚集沉淀。经绿胶鉴定我们制备的LHCI-680、LHCI-730是二聚体形式;而把PSI绿胶后再进行第二向十二烷基硫酸钠－聚丙烯酰氨凝胶电泳（SDS-PAGE）电泳，结果发现在稍强烈的绿胶增溶条件下，LHCI-730是以二聚体的形式存在，但是LHCI-680却是以单体的形式出现。这说明LHCI形成的二聚体，尤其是LHCI-680，较容易受到增溶处理而分离成单体形式，解释了以生化分离手段得到的LHCI-680的聚集形式是单体还是二聚体这个目前国际上还有有争议的问题。 3．PSI、LHCI光破坏的基本特点。 采用白光（2500 μmol•m-2•s-1）照射PSI颗粒，通过SDS-PAGE及室温吸收光谱检测光照过程中PSI复合体的变化，结果表明：去氧处理能够大大延缓PSI的光破坏，而PSI脱辅基蛋白不会发生光破坏，这说明PSI发生的光破坏可能与Chl与O2的相互作用有关。采用白光（1000 μmol•m-2•s-1、300 μmol•m-2•s-1）处理LHCI-680、LHCI-730，发现LHCI-680被破坏的速度明显快于LHCI-730被破坏的速度，这是首次在体外分离的水平上揭示了不同LHCI光破坏方面的差异。LHCI-680与LHCI-730在光破坏方面的差异可能与两种天线蛋白结合的类胡萝卜素的种类和数量不同有关，还可能与二者结合的长波长Chl的情况有关，但是具体的原因还有待于进一步的研究。 4．结合不同的捕光色素蛋白复合体（light-harvesting complex，LHC）对PSI光破坏的影响。 为了研究结合不同的捕光天线对PSI光破坏的影响，我们制备了PSI-LHCII、PSI、PSI core三种复合体。使用白光（2500 μmol•m-2•s-1）照射这三种复合体，并通过测定各复合体在光破坏过程中蛋白亚基、吸收光谱、PSI活性及P700含量的变化，对比三者光破坏的速度，结果发现PSI-LHCII在这三种复合体中光破坏速度最快，而PSI和PSI core两种复合体光破坏速度基本一致。我们推测在光照过程中部分光系统II捕光Chl a/b蛋白复合体II（light-harvesting complex II，LHCII）能够向PSI core传递能量，另外PSI-LHCII绿胶分析的结果表明发生了LHCII三聚体向单体的转变，这种强光下发生的LHCII聚合形式的转化可能是高光强下调节光能捕获的一种机制，由于植物体内具有较完整的保护系统，体内PSI-LHCII的光破坏可能与体外情况不同;另外LHCI与PSI core的解离可能发生在强光照射的早期，具有保护PSI core减少光破坏的积极作用。该部分的研究首次观察了结合不同的捕光天线对PSI光破坏的影响。

Nucleosome core histone complex isolated gently and rapidly in 2 M NaCl is octameric

A relatively stable specific complex of the chromatin core histones H2A, H2B, H3, and H4 has been obtained in 2 M NaCl/25 mM sodium phosphate buffer, pH 7.0. The histone core complex has an apparent specific volume of 0.73 ml/g. Its sedimentation coefficient was dependent on rotor speed (angular velocity, omega) and attained different stable values at low and high rotor speeds. The drop in sedimentation coefficient occurred sharply between omega 2 values of about 9 x 10(6) and 1.1 x 10(7) (radians/sec)2. The s020,w corresponding to zero angular velocity (1 atmosphere pressure) was 6.6 S +/- (SEM) 0.1 S. At high rotor speeds the value decreased to 3.8 S +/- 0.1 S. The core complex has a diffusion coefficient, D20,w, of 5.4 x 10(-7) cm2/sec and a molecular weight of 108,000 +/- (SD) 2500.

Isolation of PSI from a siphonous marine green alga, Codium fragile

Three different forms of PS I complexes were isolated from a siphonous marine green alga, Codium fragile, by Triton X-100 sucrose gradient centrifugation. Zone III had a Chl a/b>20, and designated as PS I. core complex CC I because it created only CP I band in mild PAGE. Zone IV and V had absorption at 436 and 674 nm, 467 and 650 nm, and 540 nm, suggesting the presence of Chl a, Chl b, siphonaxanthin and siphonein, Chl a/b were 3.23 and 2.4, respectively. Both CP I and CP I a bands were observed when they were subjected to mild PAGE. Therefore, Zone IV and V were different forms of PS I complexes that consisted of CC I and different amount of light-harvesting complex LHC I. Zone III contained only 66 and 56 ku peptides in SDS-PAGE, while Zone IV and V had 4 different LHC I peptides of 25, 26, 26.2 and 27.5 ku in addition to 66, 56 ku peptides. Fluorescence emission spectra showed that efficient energy transfer were kept among pigments in isolated PS I complexes. Excitation energy absorbed by Chl b, siphonaxanthin and siphonein can be transferred to Chl a.

Multiple Domains of Fission Yeast Cdc19p (MCM2) Are Required for Its Association with the Core MCM Complex

The members of the MCM protein family are essential eukaryotic DNA replication factors that form a six-member protein complex. In this study, we use antibodies to four MCM proteins to investigate the structure of and requirements for the formation of fission yeast MCM complexes in vivo, with particular regard to Cdc19p (MCM2). Gel filtration analysis shows that the MCM protein complexes are unstable and can be broken down to subcomplexes. Using coimmunoprecipitation, we find that Mis5p (MCM6) and Cdc21p (MCM4) are tightly associated with one another in a core complex with which Cdc19p loosely associates. Assembly of Cdc19p with the core depends upon Cdc21p. Interestingly, there is no obvious change in Cdc19p-containing MCM complexes through the cell cycle. Using a panel of Cdc19p mutants, we find that multiple domains of Cdc19p are required for MCM binding. These studies indicate that MCM complexes in fission yeast have distinct substructures, which may be relevant for function.

Nucleosome core protein: Asymmetric dissociation of the octamer

The octameric nucleosomal core-histone complex, (H2A)2-(H2B)2-(H3)2-(H4)2, isolated from rat liver, undergoes dissociation during gel exclusion chromatography as a result of dilution occurring in the columns. The elution pattern at pH 7.0 and 4°C showed a sharp leading peak containing all four histones but predominantly H3 and H4, and a trailing peak containing equal amounts of histones H2A and H2B. As column length was increased the area under the leading peak decreased and that under the trailing peak increased. In addition the relative positions of the two peaks varied with column length. From an analysis of the data on increase in elution volume of the leading peak in relation to column length an apparent molecular weight of 86 000 was calculated for the undissociated molecule. Its apparent molecular weight, histone composition and pattern of further dissociation in relation to column length suggest that this species is the hexamer, (H2A-H2B)-(H3)2-(H4)2. At pH 7.0 and 4°C the dissociation of the core complex appears to be as follows: (H2A)2-(H2B)2-(H3)2-(H4)2 → (H2A-H2B) + (H2A-H2B)-(H3)2-(H4)2 → 2(H2A-H2B) + (H3)2-(H4)2 This dissociation was accelerated by an increase in temperature or decrease in pH and was accompanied by marked conformational changes as judged by circular dichroism measurements.