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Sie rast, sie schleicht, sie fließt, sie tröpfelt: Obwohl der Tag immer 24 Stunden hat, nehmen wir die Zeit sehr unterschiedlich wahr. In der Kindheit tickt die innere Uhr anders als in der Rushhour des Lebens oder kurz vor dem Tod. Aber nicht nur das Alter spielt eine Rolle, sondern viele weitere Faktoren beeinflussen unser Zeitempfinden.
Ein Fahrradunfall mit einem komplizierten Knochenbruch katapultiert Autor Simon Garfield plötzlich aus der Zeit. Nachts um drei Uhr liegt er in einem abgedunkelten Krankenzimmer, bekleidet mit einem getüpfelten, hinten zugebundenen Nachthemd und fragt sich, wie lang er auf die Operation warten muss. "Ich lag wieder in einer Wiege, wo ich über die Zeit nicht mehr zu bestimmen hatte, und das brachte mich zu der Frage, inwieweit ich das überhaupt je getan hatte." ...
Laut jüdischem Kalender entstand die Welt vor genau 5778 Jahren, nach der Bibel vor 6021 Jahren. Doch als Forscher begannen, auf und in der Erde selbst nach Spuren ihres Alters zu suchen, mussten sie die Zahl immer weiter nach oben korrigieren. Nach heutigen Datierungsmethoden ist unser Planet zwischen 4,5 und 4,6 Milliarden Jahre alt.
Background: Alzheimer’s Disease (AD) is the most common form of dementia and one of the major diseases of old age, causing the impairment of cognitive functions. This disease does not only confront society with financial issues, but also puts severe stress on individuals suffering from AD and their relatives alike. One of the possible symptoms, commonly described in AD, is the impairment of learning as well as the recognition of face-name associations. Beginning at age 60, the chance to develop AD grows exponentially with increasing age, making age a major risk factor. Additionally, the e4 allele of the apolipoprotein E (APOE) polymorphism has been associated with the risk of developing AD when compared to the more common e3 allele. While strong evidence shows a stronger decline in cognitive function with rising age for e4 carriers, some studies demonstrated better cognitive function in e4 carriers at a young age.
This led to the postulation of the hypothesis of antagonistic pleiotropy of the APOE gene, wherein the e4 allele may benefit cognitive function in young carriers, yet leads to a faster decline at a later point in life, encouraging the development of cognitive dysfunction such as AD. Several functional magnetic resonance imaging (fMRI) studies, examining functional activation patterns, found APOE-related differences in key areas of episodic memory, such as the hippocampus, where e4 carriers show aberrant activation similar to AD patients. However, associative memory (encoding and retrieval of face name pairs) has not been well examined for APOE-related differences. Interaction effects of age and the APOE genotype, such as those postulated by the hypothesis of antagonistic pleiotropy, have not been addressed in face-name association tasks either.
Leading Question: Is it possible to detect interaction effects between age and APOE genotype on cognitive performance or neuronal activation patterns in healthy young and old participants during an fMRI face-name association task, supporting the hypothesis of antagonistic pleiotropy of the APOE genotype?
Methods: Participants were stratied by age, and APOE e4 carriers were randomly matched with homozygous e3 carriers. Neuropsychological examination (CVLT and CERAD) was administered. Participants underwent structural MRI analysis via voxelbased morphometry (VBM) as well as fMRI imaging during a face-name association task.
Results: Apart from strong age-related effects in cognitive function detected during neuropsychological testing, the behavioral data from the face-name association task as well as the structural MRI analysis did not show an association with the APOE genotype. Nevertheless, analysis of functional MRI data showed age- as well as APOE-dependent effects on activation patterns for the encoding and retrieval of face-name pairs, in absence of differences in cognitive performance. Further analysis showed eight clusters of significant age X APOE genotype interactions in areas previously associated with working and visual associative memory, including the fusiform gyri bilaterally. These interactions show different patterns, whereas a relative hypoactivation of young e4 carriers together with a hyperactivation of old e4 carriers is the most prominent.
Conclusions: With regard to the leading question, this study successfully found age X APOE interactions in a face-name pair retrieval task, although no interaction effects were present in the encoding task, structural analysis, or cognitive performance. The agemediated effect of the APOE e4 allele on functional activation patterns may be explained by the compensatory hypothesis, describing a relative hyperactivation of old e4 carriers as compensatory, and interpreting a relative hypoactivation of younger e4 participants as reduced effort to achieve the same cognitive performance as non carriers.
These findings present further evidence of an antagonistic pleiotropy of the APOE genotype, showing age-dependent effects of the e4 allele even in healthy carriers. Nevertheless, previously described differences in cognitive performance and brain structure, even in young participants, were not found. On the contrary, functional MRI analysis showed APOE-related differences in young and old participants, suggesting that this modality may be more sensitive in detecting APOE-mediated changes. Among the clusters, demonstrating an interaction effect, the fusiform gyri were most prominent, which might be due to its important role in visual associative memory. As previous studies indicate an early and strong involvement of this area due to AD pathology, this interaction effect of age and APOE genotype in healthy participants underlines the importance of this region in the development of AD, and should be the focus of further research. However, this research is also required to determine, how exactly the APOE genotype influences brain function in healthy humans, and to clarify its relationship to pathological processes facilitating the development of AD.
The Earth’s surface condition we find today is a result of long exposure to metabolism of life forms. Particularly, molecular oxygen in the atmosphere is a feature which developed over time. The first substantial and lasting rise of atmospheric oxygen level happened ≈ 2.5 Ga ago, but localities are reported where transiently elevated oxygen levels appeared before this time-point. To trace the timing and circumstances of the earliest availability of free oxygen in the atmosphere is important to understand the habitats of early microbial life forms on Earth.
This thesis focuses to obtain information of oxygen levels and the related atmospheric cycling of metals in sediments of the 3.5 to 3.2 Ga Barberton Greenstone Belt. First, as iron was a ubiquitous constituent of Archean seawater, I investigated its isotopic composition in minerals of chemical sediments. Hereby, I tried to resolve the changes within the water basin on small scale sedimentary sequence cycles. Second, I focused on the minor constituents of Archean seawater. The Re-Os geochronologic system and the abundance patterns of the platinum-group elements were chosen to integrate information of oxygen promoted weathering of a large source area. To integrate information of a large time interval, the isotopes of uranium were investigated over a large stratigraphic section.
The two key findings of this thesis are:
• Quantitative oxidation of ferrous iron in surface layers of Paleoarchean seawater occurred during the onset and termination of hydrothermal FeIIaq delivery into shallow waters.
• Paleoarchean sedimentary successions of the Barberton Greenstone Belt lack any evidence of transient basin-scale oxygenation.
The Manzimnyama Iron Formation (IF, Fig Tree Group, Barberton Greenstone Belt, South Africa) has been deciphered to exist of cyclic stacks of lithostratigraphic units with varying amounts of iron oxide and carbonate minerals. In-situ femtosecond-Laser-Ablation ICP-MS iron isotope measurements showed that the majority of siderite (γ56Fe ≈ −0.5 ‰) precipitated directly from seawater of γ56Fe ≈ 0 ‰. Ferric iron from the surface layers is preserved in ≤ 1μ m hematite and in magnetite that has been grown within the consolidated sediment. During FeIIaq events, fine-grained hematite (γ56Fe ≈ 2.2 ‰) and magnetite (γ56Fe 0.5 to 0.8 ‰) indicate oxygen levels in surface waters of lower than 0.0002 μM. Upon onset and termination of iron oxide abundance, magnetite with γ56Fe ≈ 0 ‰ indicates that low concentrations of FeIIaq in surface waters were oxidized quantitatively. These observations demonstrate the existence of iron oxidation in Paleoarchean surface waters independent of FeIIaq concentration. This is the first investigation of Paleoarchean IF showing that lithostratigraphic cyclicity can be traced in iron isotopic composition of oxide minerals.
ID-ICP-MS measurement of Re, Ir, Ru, Pt and Pd, trace element (SF-ICP-MS) and ID-MCICP- MS uranium isotope determination have been applied to carbonaceous shale of the Mapepe Fm. (Fig Tree Group) after inverse Aqua Regia leaching and bulk digestion. The sediments reveal a silicified fraction which exhibits a seawater REE signature and a mixture of detrital and meteoritic PGE. Neither enrichment of the redox-sensitive elements Re or Mo nor fractionated uranium isotopes have been found on a stratigraphic interval of several hundred meters. The non-silica fraction shows no depletion of Re which indicates that the detrital material had no contact to oxidizing fluids. ID-TIMS measurements of Re and Os after the CrO3-SO4 Carius Tube method of two sample intervals showed that the Re-Os isotopic systems of the non-silica fractions are identical to two komatiite occurrences. Weltevreden Fm. and Komati Fm. rocks were uplifted, eroded and transported to the deep part of the sedimentary basin without any change to the Re-Os system. Negative fractionated uranium isotopes (γ238U = −0.41 ± 0.01 ‰) associated with detrital Ba-Cr-U occurrences suggest the existence of distal redox-processes that involve uranium species. This study demonstrates that over the time of exposure and deposition of the Mapepe Fm. sedimentation, free oxygen was not available for weathering in the catchment area.