Functional dna nanostructures for in vitro biosensing in live cells

DNA is a fascinating biomolecule that is well known for its genetic role in living systems. The emerging area of DNA nanotechnology provides an alternative view that exploits unparallel self-assembly ability of DNA molecules for material use of DNA. Although many reports exist on the results of DNA self-assembling systems, still few of them focus on the in vitro study about the function of such DNA nanostructures in live cells. Due to this, there are still a limited research about the in vitro functionality of such designs. To address an aspect of this issue, we have designed, synthesized and characterized two multifunctional fluorescencent nanobiosensors by DNA self-assembling. Each structure was designed and implemented to be introduced in live cells in order to give information on their functioning in real-time. Computational tools were used in order to design a graphic model of two new DNA motifs and also to obtain the specific sequences to all the ssDNA molecules. By thermal self-assembly techniques we have successfully synthesized the structure and corroborate their formation by the PAGE technique. In addition, we have established the conditions to characterize their structural conformation change when they perform their sensor response. The sensing behavior was also accomplished by fluorescence spectroscopy techniques; FRET evaluation and fluorescence microscopy imaging. Providing the evidence about their adequate sensing performance outside and inside the cells detected in real-time. In a preliminary evaluation we have tried to show the in vitro functionality of our structures in different cancer cell lines with the ability to perform local sensing responses. Our findings suggest that DNA sensor nanostructures could serve as a platform to exploit further therapeutic achievements in live cells.

Funktionelle Analyse der Plasmamembran-Ca 2+-ATPase 2 -PMCA2- in Modellen der Neurodegeneration

Calcium (Ca2+) ist ein ubiquitär vorkommendes Signalmolekül, das an der Regulation zahlreicher zellulärer Prozesse, von der Proliferation bis zum programmierten Zelltod, beteiligt ist. Daher müssen die intrazellulären Ca2+-Spiegel streng kontrolliert werden. Veränderungen der Ca2+-Homöostase während der altersassoziierten Neurodegeneration können dazu beitragen, dass Neuronen vulnerabler sind. So wurden erhöhte Ca2+-Konzentrationen in gealterten Neuronen, begleitet von einer erhöhten Vulnerabilität, beobachtet (Hajieva et al., 2009a). Weiterhin wird angenommen, dass der selektive Untergang von dopaminergen Neuronen bei der Parkinson Erkrankung auf eine erhöhte Ca2+-Last zurückzuführen sein könnte, da diese Neuronen einem ständigen Ca2+-Influx,rnaufgrund einer besonderen Isoform (CaV 1.3) spannungsgesteuerter Ca2+-Kanäle des L-Typs, ausgesetzt sind (Chan et al., 2007). Bislang wurden die molekularen Mechanismen, die einem Ca2+-Anstieg zu Grunde liegen und dessen Auswirkung jedoch nicht vollständig aufgeklärt und daher in der vorliegenden Arbeit untersucht. Um Veränderungen der Ca2+-Homöostase während der altersassoziiertenrnNeurodegeneration zu analysieren wurden primäre Mittelhirnzellen aus Rattenembryonen und SH-SY5Y-Neuroblastomazellen mit dem Neurotoxin 1-Methyl-4-Phenyl-Pyridin (MPP+), das bei der Etablierung von Modellen der Parkinson-Erkrankung breite Anwendung findet, behandelt. Veränderungen der intrazellulären Ca2+-Konzentration wurden mit einem auf dem grün fluoreszierenden Protein (GFP)-basierten Ca2+-Indikator,rn„Cameleon cpYC 3.6“ (Nagai et al., 2004), ermittelt. Dabei wurde in dieser Arbeit gezeigt, dass MPP+ die Abregulation der neuronenspezifischen ATP-abhängigen Ca2+-Pumpe der Plasmamembran (PMCA2) induziert, die mit der Ca2+-ATPase des endoplasmatischen Retikulums (SERCA) und dem Na+/Ca2+-Austauscher (NCX) das zelluläre Ca2+-Effluxsystem bildet, was zu einer erhöhten zytosolischen Ca2+-Konzentration führt. Die PMCA2-Abnahme wurde sowohl auf Transkriptionsebene als auch auf Proteinebene demonstriert, während keine signifikanten Veränderungen der SERCA- und NCX-Proteinmengen festgestellt wurden. Als Ursache der Reduktion der PMCA2-Expression wurde eine Abnahme des Transkriptionsfaktors Phospho-CREB ermittelt, dessen Phosphorylierungsstatus abhängig von der Proteinkinase A (PKA) war. Dieser Mechanismus wurde einerseits unter MPP+-Einfluss und andererseits vermittelt durch endogene molekulare Modulatoren gezeigt. Interessanterweise konnten die durch MPP+ induzierte PMCA2-Abregulation und der zytosolische Ca2+-Anstieg durch die Aktivierung der PKA verhindert werden. Parallel dazu wurde eine MPP+-abhängige verringerte mitochondriale Ca2+-Konzentration nachgewiesen, welche mit einer Abnahme des mitochondrialen Membranpotentials korrelierte. Darüber hinaus kam es als Folge der PMCA2-Abnahme zu einem verminderten neuronalen Überleben.rnVeränderungen der Ca2+-Homöostase wurden auch während der normalen Alterung inrnprimären Fibroblasten und bei Mäusen nachgewiesen. Dabei wurden verringerte PMCA und SERCA-Proteinmengen in gealterten Fibroblasten, einhergehend mit einem Anstieg der zytosolischen Ca2+-Konzentration demonstriert. Weiterhin wurden verringerte PMCA2-Proteinmengen im Mittelhirn von gealterten Mäusen (C57B/6) detektiert.rnDer zelluläre Ca2+-Efflux ist somit sowohl im Zuge der physiologischen Alterung als auch in einem altersbezogenen Krankheitsmodell beeinträchtigt, was das neuronale Überleben beeinflussen kann. In zukünftige Studien soll aufgeklärt werden, welche Auswirkungen einer PMCA2-Reduktion genau zu dem Verlust von Neuronen führen bzw. ob durch eine PMCA2-Überexpression neurodegenerative Prozesse verhindert werden können.

Detrital Zircon Evidence for Non-Laurentian Provenance, Mesoproterozoic (ca. 1490-1450 Ma) Deposition and Orogenesis in a Reconstructed Orogenic Belt, Northern New Mexico, USA: Defining the Picuris Orogeny

Detrital zircon and igneous zircon U-Pb ages are reported from Proterozoic metamorphic rocks in northern New Mexico. These data give new insight into the provenance and depositional age of a >3-km-thick metasedimentary succession and help resolve the timing of orogenesis within an area of overlapping accretionary orogens and thermal events related to the Proterozoic tectonic evolution of southwest Laurentia. Three samples from the Paleoproterozoic Vadito Group yield narrow, unimodal detrital zircon age spectra with peak ages near 1710 Ma. Igneous rocks that intrude the Vadito Group include the Cerro Alto metadacite, the Picuris Pueblo granite, and the Penasco quartz monzonite and yield crystallization ages of 1710 +/- 10 Ma, 1699 +/- 3 Ma, and 1450 +/- 10 Ma, respectively. Within the overlying Hondo Group, a metamorphosed tuff layer from the Pilar Formation yields an age of 1488 +/- 6 Ma and represents the first direct depositional age constraint on any part of the Proterozoic metasedimentary succession in northern New Mexico. Detrital zircon from the overlying Piedra Lumbre Formation yield a minimum age peak of 1475 Ma, and similar to 60 grains (similar to 25%) yield ages between 1500 Ma and 1600 Ma, possibly representing non-Laurentian detritus originating from Australia and/or Antarctica. Detrital zircons from the basal metaconglomerate and the middle quartzite member of the Marquenas Formation yield minimum age peaks of 1472 Ma and 1471 Ma, consistent with earlier results. We interpret the onset of ca. 1490-1450 Ma deposition followed by tectonic burial, regional Al2SiO5 triple-point metamorphism, and ductile deformation at depths of 12-18 km to reflect a Mesoproterozoic contractional orogenic event, possibly related to the final suturing of the Mazatzal crustal province to the southern margin of Laurentia. We propose to call this event the Picuris orogeny.

Association of the (CA)n repeat polymorphism of insulin-like growth factor-I and -202 A/C IGF-binding protein-3 promoter polymorphism with adult height in patients with severe growth hormone deficiency

A number of mathematical models for predicting growth and final height outcome have been proposed to enable the clinician to 'individualize' growth-promoting treatment. However, despite optimizing these models, many patients with isolated growth hormone deficiency (IGHD) do not reach their target height. The aim of this study was to analyse the impact of polymorphic genotypes [CA repeat promoter polymorphism of insulin-like growth factor-I (IGF-I) and the -202 A/C promoter polymorphism of IGF-Binding Protein-3 (IGFBP-3)] on variable growth factors as well as final height in severe IGHD following GH treatment. DESIGN, PATIENTS AND CONTROLS: One hundred seventy eight (IGF-I) and 167 (IGFBP-3) subjects with severe growth retardation because of IGHD were studied. In addition, the various genotypes were also studied in a healthy control group of 211 subjects.

Detrital Zircon Evidence for Mixing of Mazatzal Province Age Detritus With Yavapai Age (ca. 1700-1740 Ma) and Older Detritus in the ca. 1650 Ma Mazatzal Province of Central New Mexico, USA

Preliminary detrital zircon age distributions from Mazatzal crustal province quartzite and schist exposed in the Manzano Mountains and Pedernal Hills of central New Mexico are consistent with a mixture of detritus from Mazatzal age (ca. 1650 Ma), Yavapai age (ca. 1720 Ma.), and older sources. A quartzite sample from the Blue Springs Formation in the Manzano Mountains yielding 67 concordant grain analyses shows two dominant age peaks of 1737 Ma and 1791 Ma with a minimum peak age of 1652 Ma. Quartzite and micaceous quartzite samples from near Pedernal Peak give unimodal peak ages of ca. 1695 Ma and 1738 Ma with minimum detrital zircon ages of ca. 1625 Ma and 1680 Ma, respectively. A schist sample from the southern exposures of the Pedernal Hills area gives a unimodal peak age of 1680 Ma with a minimum age of ca. 1635 Ma. Minor amounts of older detritus (>1800 Ma) possibly reflect Trans-Hudson, Wyoming, Mojave Province, and older Archean sources and aid in locating potential source terrains for these detrital zircon. The Blue Springs Formation metarhyolite from near the top of the Proterozoic section in the Manzano Mountains yields 71 concordant grains that show a preliminary U-Pb zircon crystallization age of 1621 ¿ 5 Ma, which provides a minimum age constraint for deposition in the Manzano Mountains. Normalized probability plots from this study are similar to previously reported age distributions in the Burro and San Andres Mountains in southern New Mexico and suggest that Yavapai Province age detritus was deposited and intermingled with Mazatzal Province age detritus across much of the Mazatzal crustal province in New Mexico. This data shows that the tectonic evolution of southwestern Laurentia is associated with multiple orogenic events. Regional metamorphism and deformation in the area must postdate the Mazatzal Orogeny and ca. 1610 Ma ¿ 1620 Ma rhyolite crystallization and is attributed to the Mesoproterozoic ca. 1400 ¿ 1480 Ma Picuris Orogeny.

Agonist specific L-type Ca(2+)-current stimulation in ventricular myocytes by a novel steroid-like compound

In cardiac muscle the amplitude of Ca(2+) transients can be increased by enhancing Ca(2+) influx. Among the processes leading to increased Ca(2+) influx, agonists of the L-type Ca(2+)-channel can play an important role. Known pharmacological Ca(2+)-channel agonists act on different binding sites on the channel protein, which may lead not only to enhanced peak currents, but also to distinct changes in other biophysical characteristics of the current. In this study, membrane currents were recorded with the patch-clamp technique in the whole-cell configuration in guinea pig isolated ventricular myocytes in combination with confocal fluorescence Ca(2+) imaging techniques and a variety of pharmacological tools. Testing a new positive inotropic steroid-like compound, we found that it increased the L-type Ca(2+)-current by 2.5-fold by shifting the voltage-dependence of activation by 20.2 mV towards negative potentials. The dose-response relationship revealed two vastly different affinities (EC(50(high-affinity))=4.5+/-1.7 nM, EC(50(low-affinity))=8.0+/-1.1 microM) exhibiting differential pharmacological interactions with three classes of Ca(2+)-current antagonists, suggesting more than one binding site on the channel protein. Therefore, we identified and characterized a novel positive inotropic compound (F90927) as a member of a new class of Ca(2+)-channel agonists exhibiting unique features, which set it apart from other presently known L-type Ca(2+)-channel agonists.

Ca(2+) release from the sarcoplasmic reticulum activated by the low affinity Ca(2+) chelator TPEN in ventricular myocytes

The Ca(2+) content of the sarcoplasmic reticulum (SR) of cardiac myocytes is thought to play a role in the regulation and termination of SR Ca(2+) release through the ryanodine receptors (RyRs). Experimentally altering the amount of Ca(2+) within the SR with the membrane-permeant low affinity Ca(2+) chelator TPEN could improve our understanding of the mechanism(s) by which SR Ca(2+) content and SR Ca(2+) depletion can influence Ca(2+) release sensitivity and termination. We applied laser-scanning confocal microscopy to examine SR Ca(2+) release in freshly isolated ventricular myocytes loaded with fluo-3, while simultaneously recording membrane currents using the whole-cell patch-clamp technique. Following application of TPEN, local spontaneous Ca(2+) releases increased in frequency and developed into cell-wide Ca(2+) waves. SR Ca(2+) load after TPEN application was found to be reduced to about 60% of control. Isolated cardiac RyRs reconstituted into lipid bilayers exhibited a two-fold increase of their open probability. At the low concentration used (20-40muM), TPEN did not significantly inhibit the SR-Ca(2+)-ATPase in SR vesicles. These results indicate that TPEN, traditionally used as a low affinity Ca(2+) chelator in intracellular Ca(2+) stores, may also act directly on the RyRs inducing an increase in their open probability. This in turn results in an increased Ca(2+) leak from the SR leading to its Ca(2+) depletion. Lowering of SR Ca(2+) content may be a mechanism underlying the recently reported cardioprotective and antiarrhythmic features of TPEN.