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In this study, I investigate the crustal and upper mantle velocity structure beneath the Rwenzori Mountains in western Uganda. This mountain range is situated within the western branch of the East African Rift and reaches altitudes of more than 5000 m. I use four different approaches that belong to the travel-time tomography method. The first approach is based on the isotropic tomographic inversion of local data, which contain information about 2053 earthquakes recorded by a network of up to 35 stations covering an area of 140×90 km2. The LOTOS-09 algorithm described here is used to realize this approach. The second approach is based on the anisotropic tomographic inversion of the same local dataset. This method employs the tomographic code ANITA, developed with my participation, which provides 3D anisotropic P and isotropic S velocity distributions based on P and S travel-times from local seismicity. For the P anisotropic model, four parameters for each parameterization cell are determined. This represents an orthorhombic anisotropy with one vertically-oriented predefined direction. Three of the parameters describe slowness variations along three horizontal orientations with azimuths of 0°, 60° and 120°, and one is a perturbation along the vertical axis. The third approach is based on tomographic inversion of the teleseismic data, which contain information about the traveltimes of P-waves coming from 284 teleseismic events recorded by the seismic network stations. The TELELOTOS code, which is my own modification of the LOTOS-09 algorithm, is used in this approach. The TELELOTOS code is designed to iteratively invert the local and/or teleseismic datasets. Finally, I present the results of the new tomographic approach, which is based on the simultaneous inversion of the joint local and teleseismic data. The simultaneous use of these datasets for the tomographic inversion has several advantages. In this case, the velocity structure in the study area can be resolved as deep as in the teleseismic approach. At the same time, in the upper part of the study volume, the resolution of the obtained models is as good as in the local tomography. The TELELOTOS algorithm is used to perform the joint tomographic inversion. Special attention is paid in this work to synthetic testing. A number of different synthetic and real data tests are performed to estimate the resolution ability and robustness of the obtained models. In particular, synthetic tests have shown that the results of the anisotropic tomographic inversion of the local data have to be considered as unsatisfactory. For all approaches used in this study, I present synthetic models that reproduce the same pattern of anomalies as that obtained by inverting the real data. These models are used to interpret the results and estimate the real amplitudes of the obtained anomalies. The obtained models exhibit a relatively strong negative P anomaly (up to -10%) beneath the Rwenzori Mountains. Low velocities are found in the northeastern part of the array at shallower depths and are most likely related to sedimentary deposits, while higher velocities are found beneath the eastern rift shoulder and are thought to be related to old cratonic crust. The presence of low velocities in the northwestern part of the array may be caused by a magmatic intrusion beneath the Buranga hot springs. Relatively low velocities were observed within the lower crust and upper mantle in the western and southern parts of the study area (beneath the rift valley and the entire length of the Rwenzori range). The higher amplitude of the low-velocity anomaly in the south can be related to the thinner lithosphere in the southern part of the Albertine rift. In the center of the study area, a small negative anomaly is observed, with the intensity increasing with depth. This anomaly is presumably related to a fluids rising up from a plume branch in the deeper part of the mantle. According to the interpretation of the local earthquake distribution, the Rwenzori Mountains are located between two rift valleys with flanks marked by normal faults. The Rwenzori block is bounded by thrust faults that are probably due to compression.
An eclogite barometer has profound importance in the study of upper mantle processes and potential application to diamond prospecting. Studies on the partitioning of Li between clinopyroxene (cpx) and garnet (grt) in natural samples have shown that this particular element is very sensitive to changes in pressure and could be calibrated as the barometer demanded for bimineralic eclogites. Experiments were performed from 4 to 13 GPa and 1100 to 1400°C in the CMAS (CaO, MgO, Al2O3, SiO2) system with Li added as Li3PO4 to quantify this pressure dependence into a barometer expressed in the following equation: P= (0.00255*T-lnKd)/0.2351 where P is in GPa, T is in °C and Kd is defined as the partition coefficient of Li (in ppm) between clinopyroxene and garnet. The experimental pressures are reproduced to ± 0.38 GPa (1σ) by this equation. This barometer is strictly applicable only to CMAS. Experiments at 1300°C, 8-12 GPa showed that Henry’s Law is fulfilled for Li partitioning between cpx and grt in the concentration range of approximately 0.01 – 1 wt% Li. Direct application of the equation to experiments in natural systems performed at 1300°C from 4 GPa to 13 GPa consistently overestimates pressures by approximately 2 GPa. Our previous experiments in the system CaO-MgO-Al2O3-SiO2 + Li3PO4 showed that the partitioning of Li between garnet and clinopyroxene is pressure dependent in eclogitic bulk compositions. This supports experimentally the hypothesis of Seitz et al. (2003), based on the analysis of Li in eclogitic xenoliths and inclusions in diamond, that the partitioning of this particular element between clinopyroxene and garnet is very sensitive to changes in pressure and could be calibrated as a barometer for bimineralic eclogites. In order to calibrate this pressure dependence into a barometer, experiments were performed in natural systems using starting materials sourced from a well preserved eclogitic xenolith from the Roberts Victor kimberlite pipe (South Africa) to extrapolate our findings in CMAS to natural systems. Sixteen multianvil experiments were performed from 4-13 GPa and 1100-1500°C. Our findings reinforced the general trend we observed in the CMAS system, that KdLi cpx-grt for Li decreases with increasing P, and that at P ≥ 12 GPa, garnet is able to incorporate more Li than clinopyroxene. Multiple linear regression was applied to our experimental results to create the barometer: P = (0.000963*T – ln KdLi cpx-grt + 1.581) / 0.252 Where P is pressure in GPa, T is temperature in °C and KdLi cpx-grt is defined as the partitioning coefficient of Li obtained by dividing the concentration of Li in cpx by the concentration of Li in garnet. This barometer reproduces the experimental conditions to ± 0.2 GPa. It is applicable to eclogitic xenoliths, to garnet pyroxenites and to peridotitic and eclogitic inclusions in diamond. Application of the barometer to diamond bearing xenoliths results in pressures in the diamond stability field. Clinopyroxene is easily corrupted in xenoliths and also preferentially takes in Li during short lived metasomatic processes. Care must be taken therefore to analyse primary, unaltered clinopyroxene. Our preliminary application to natural samples shows that the barometer can be applied beyond the experimental range to pressures down to 3 GPa. Seventeen eclogitic xenoliths were chosen from a sample set of greater than 200 for their fresh microscopic and macroscopic appearance and were analyzed for Li content in coexisting garnet (grt) and clinopyroxene (cpx). These samples can be subdivided into two groups on the basis of Mg in cpx (cpfu: cations per formula unit, based on 6 oxygens): Group 1 with Mg > 0.75, and Group 2 with Mg < 0.75. Group 1 xenoliths show lower Li contents in both grt and cpx compared to Group 2. The Li barom ter calibrated in Hanrahan et al. (2009b)/Chapter 3 was applied to these samples as well as available literature data to obtain pressures of provenance - Group 2 xenoliths often provide pressures that appear unrealistic for eclogitic xenoliths. In light of observed crystal chemical relations in the natural samples, a new fitting procedure was applied to the experimental data presented in Chapter 3. This new fit appears to be more realistic than the previous fit, although a strong relationship with Mg# remains present, suggesting that Li-barometry is, at present, only applicable to Mg-rich eclogites. Inclusions in diamond, with the exception of eclogitic inclusions of coexisting majorite and cpx, often yield pressures that are inconsistent with the pressures required for diamond formation. Although an interesting observation when comparing all of the data is that inclusions in diamond have significantly higher average Li concentrations compared to xenoliths, which suggests that Li is highly present in the fluids from which diamonds form in the mantle, an observation which was previously made for the deep mantle as a result of high Li in ferropericlase inclusions in diamond (Seitz et al. 2003).
The present PhD-thesis was prepared within subproject B8 of the DFG-Sonderforschungsbereich (SFB) 641 “The Tropospheric Ice Phase”. The subproject B8 was entitled “Interactions of volatile organic compounds with airborne ice crystals”. Results of previous studies have shown that various volatile organic compounds (VOC) and semivolatile organic compounds (SVOC) are incorporated into the atmospheric ice phase and several uptake mechanisms are discussed in the literature. The aim of this study was to identify the dominating VOC and SVOC in airborne snow collected at Jungfraujoch in the Swiss Alps (3580 m asl) and to study in laboratory experiments the uptake mechanism of organic compounds into snow and ice. For this purpose an analytical method to analyse freshly fallen snow samples was developed and evaluated in a first step. The method consists of headspace (HS) solid phase dynamic extraction (SPDE) followed by gas chromatography combined with mass spectrometry (GC/MS). During the extraction process a new cooling device was successfully integrated into the HS-SPDE-GC/MS method to enhance the extraction yield. Extraction and desorption parameters such as the number of extraction cycles, extraction temperature, desorption volume and desorption flow rate have been optimized. Detection limits for benzene, toluene, ethylbenzene, m-, p-, o- xylene (BTEX) ranged from 19 ng L-1 (benzene) to 30 ng L-1 (m/p-xylene), while those for C6-C10 n-aldehydes ranged from 21 ng L-1 (n-heptanal) to 63 ng L-1 (n-hexanal). Furthermore, freshly fallen snow samples were collected at the High Altitude Research Station Jungfraujoch (3580 m asl, Switzerland) during the field campaigns “Cloud and aerosol characterization experiment” (CLACE) 4 and 5 in February and March 2005 and 2006, respectively. Freshly fallen snow samples collected directly in-cloud on a high altitude remote location were used as approximation of airborne ice crystals since sampling of airborne ice crystals in quantities sufficient for analysis of individual organic compounds is not yet possible. In the collected snow samples a wide range of organic compounds were identified, namely BTEX, n-aldehydes (C6-C10), terpenes, chlorinated hydrocarbons and alkylated monoaromatics. The most abundant organic compounds in snow samples from Jungfaujoch during CLACE 4 and 5 were n-hexanal with a median concentration of 1.324 μg L-1 (CLACE 5) followed by n-nonanal (CLACE 5) with a median concentration of 1.239 μg L-1. High concentration variations of the analytes in snow samples collected at the same time at the same place argue for a heterogeneous composition of snow and ice. Several indicators were found that the origin of the n-aldehydes in the snow can be attributed to direct biogenic emissions from vegetation and indirect biogenic emissions through photochemical oxidation of fatty acids and alkenes. In a second step laboratory experiments were carried out to clarify the uptake mechanism of volatile and semivolatile organic compounds into snow/ice. Organic compounds can be incorporated into the atmospheric ice phase either by the process of gas scavenging, liquid scavenging (riming) or particle scavenging. Gas scavenging (incorporation of the organic compounds from the gas phase during growing of ice crystals) revealed to be ineffective based on previous laboratory experiments in which ice crystals were growing in the presence of aromatic hydrocarbons (BTEX) in the gas phase. In the present study the process of liquid scavenging (riming) was investigated in the laboratory using aqueous standard solutions containing BTEX, naldehydes (C6-C10), methyl tert-butyl ether (MTBE) and ethyl tert-butyl ether (ETBE). The headspace above the standard solution was sampled after adjusting the aqueous solutions to definite temperatures by use of a thermostat. Measurement were carried out at 25°C, 15°C and 5°C (water), -5°C and -15°C (supercooled water) and -25°C (ice). Results have shown that the known trend of lower gas phase concentrations over water concomitant with lower temperatures (Henry’s Law) is only valid for temperatures above 0°C. At temperature below 0°C, increasing concentrations of the analytes (BTEX, MTBE, ETBE and n-aldehydes) were determined in the gas phase together with decreasing temperatures. Dimensionless Henry’s law coefficients (KAW) were calculated from the concentrations of the organic compounds in the headspace above the standard solutions at temperatures between 25°C and -25°C. The observed inversion of Henry’s law coefficients of volatile and semivolatile organic compounds at a water temperature of approximately 0°C is explained by the formation of ordered zones of H2O molecules in supercooled water called “ice-like-clusters”. Together with decreasing temperatures the degree of formation of ordered zones increases which results in the removal of the organic molecules from the liquid phase and transfer into the gas phase. At a temperature of -25°C the supercooled water is converted into ice and a further significant increase of the gas phase concentrations of hydrophobic compounds such as BTEX is observed. In comparison, less hydrophobic compounds such as MTBE, ETBE and n-aldehydes are detected in lower amounts in the gas phase above the water/ice phase due to the higher water solubility and lower Henry coefficients compared to BTEX. The results show that in the absence of particles the uptake of BTEX MTBE, ETBE and C6-C10-naldehydes into ice not enhanced during freezing of a supercooled liquid, since at -25°C for these analytes the concentrations in the gas phase are higher at -25°C (ice) compared with -15°C (supercooled liquid). The heterogeneous distribution of BTEX and n-aldehydes concentrations in snow samples collected during the CLACE field campaigns suggests that adsorption of the organic compounds to particles followed by incorporation of the particles into the snow and ice might play a major role in the uptake process of organic compounds into snow and ice. To increase the knowledge about uptake processes of organic compounds into snow and ice further experiments are required with should include aerosol particles in the experimental setup to evaluate the influence of particle scavenging in the uptake processes.
Delthyridoid spiriferids are characterized by a global abundance and fast evolution during Silurian and Devonian, and, therefore, are used as important biostratigraphical and palaeobiogeographical tools. In this work, delthyridoid brachiopod faunas from different regions of today’s world, resp., of different palaeobiogeographical units, are compared side-by-side to investigate their phylogenetic relationships and to improve, in a second step, the palaeobiogeography from Late Silurian to Early Eifelian time. A new systematics of Delthyridoidae is established which is more complicated than hitherto assumed. The results of this study are mainly based on direct comparison of articulated and isolated brachiopod shells, external and internal moulds, as well as latex casts and serial sections. The computer supported cladistic analyses have turned out not to be useful due to different kinds of preservation resulting in an incomplete matrix which is insufficient for reliable cladograms. A further problem in terms of cladistical analyses are various convergences during the evolution of spiriferids. Many characters evolved independently from each other at different times in each lineage so that autapomorphies are hardly or not at all recognizable. As a result, families and genera are only definable by a combination of characters rather than by a single or a few autapomorphies. As a new method, 3D reconstruction from serial sections is introduced which made it possible for the first time to compare directly mouldic and shelly material. Preliminary results are presented herein. Statistical analyses of measurements taken from new taxa are made but regarded as a descriptive argument rather than a deciding factor for taxonmy due to incomplete preservation and/or tectonic deformation. Brachiopods, especially type material, from collections of different institutions and museums are studied as well as personal material, whenever possible collected from topotype outcrops. Emended diagnoses, if necessary, from family to species level are given. During this work several new taxa have been erected: 7 new families: Australospiriferidae, Murchisonispiriferidae, Orientospiriferidae, Otospiriferidae, Patriaspiriferidae, Rostrospiriferidae, and Trigonospiriferidae; 6 new genera, 1 of these in open nomenclature: Cyclopterospirifer, Hallispirifer, Parlinispirifer, Murchisonispirifer, Shujiapingensispirifer, and gen. nov. B; and 3 new species: Patriaspirifer merriami, Patriaspirifer johnsoni, and Murchisonispirifer feldmani; 1 taxon is defined as nomen novum: Orientospirifer nakaolingensis wani. In the framework of this project, 2 families: Filispiriferidae and Multispiriferidae; 1 subfamily: Multiplicatispiriferinae, 6 genera, 1 of them in open nomenclature: Frequentispirifer, Leonispirifer, Multiplicatispirifer, Ovetensispirifer, Turcispirifer, and Gen. A; and 9 new species, 3 of them in open nomenclature: Filispirifer hamadae, Leonispirifer leonensis, Multiplicatispirifer foumzguidensis, Oventensispirifer novascotianus, Quiringites arensentiae, Turcispirifer turciae, Multiplicatispirifer cf. foumzguidensis, Quiringites cf. arensentiae, and ?Turcispirifer sp. A which have already been established are also described in this work. The brachiopod faunas studied consist of externally very similar spiriferids which have been identified as same genera, species, or even subspecies in earlier times. These forms are considered as 6 distinct morphotypes Howellella-, Arduspirifer-, Acrospirifer-, Euryspirifer-, Paraspirifer-, and Multiplicatispirifer-like morphotypes, which are briefly introduced. The new systematics is characterized by different clades, the European/North African delthyridoid spiriferid clade, the North American delthyridoid spiriferid clade, the Asian delthyridoid spiriferid clade, the Malvinokaffric delthyridoid spiriferid clade, and the delthyridoid multiplicated spiriferid clade. Each of them is described in a cladistic and in a phylogenetic way. Their phylogenetic relationship sheds new light on palaeobiogeographical interpretations for the different stages from Late Silurian to early Middle Devonian time. A tendency for increasing endemicity is seen until the end of the Early Emsian, which is interrupted by short term regional faunal exchange within a province or within a realm, followed by a loss of endemicity resulting in global distribution of brachiopod genera until the end of Givetian time. The Old World Realm is re-defined due to the lack of phylogenetic relationship between its faunas and subdivided into the European Realm, consisting of the Gondwanan and Avalonian provinces, and the Asian Realm, consisting of the Siberian, Sino, and Mongolian provinces. A reconstruction of Lower Devonian palaeobiographical map is introduced.
NASAs Stardust Mission ist die erste Mission, die - nach den Apollo Missionen zum Mond - Material von einem extraterrestrischen Körper erfolgreich für die Untersuchung auf der Erde, zurückgebracht hat. Desweiteren konnten erfolgreich Proben von einem Interstellaren Partikelstrom aufgesammelt werden, der das Sonnensystem derzeit passiert. Die Mission erlaubt einen Einblick in die Beschaffenheit der Kometenpartikel, die Rolle von Kometen im Sonnensystem sowie den Eintrag von Staub in die Zodiakalwolke. Desweiteren erlaubt die Analyse der Kometenpartikel den direkten Vergleich zu bereits untersuchten Meteoriten und Interplanetaren Staub Partikeln (IDPs) die auf der Erde bzw. deren Stratosphäre gesammelt wurden. Stardust ist die vierte ”Discovery” Mission und wurde am 7. Februar 1999 gestartet. Während des Fluges zum Kometen 81P/Wild 2 wurde ein interstellarer Partikelstrom beprobt und der Asteroid Annefrank passiert. Nach fünf Jahren kam es zum Zusammentreffen mit dem Kometen 81P/Wild 2 und über fünf Minuten, wurden Proben mit einer Auffangvorrichtung eingesammelt. Es dauerte weitere zwei Jahre bis die Stardust Sonde die Proben erfolgreich zur Erde zurückgebracht hat und zur Untersuchung freigegeben wurden. Interstellare und kometare Partikel wurden mit einer tennisschlägerartigen Auffangvorrichtung eingefangen, die aus einer Vielzahl von Aerogel Zellen aufgebaut ist. Das für die Stardust Mission verwendete Aerogel besteht aus SiO2 dessen dendritische Struktur zu 99,8 % aus Luft (Poren) besteht. Dadurch erscheint es nahezu transparent, was die optische Suche mit Mikroskopen nach den Einschlagsspuren der Körner vereinfacht. Die jeweiligen Partikel wurden auf unterschiedlichen Seiten der Vorrichtung eingefangen, da unterschiedliche Eigenschaften des Aerogels notwendig waren und um sie später voneinander unterscheiden zu können. Die Seite, in der die Kometenpartikel eingefangen wurde, musste Körner mit unterschiedlichen Grössen, Morphologien und niedrigeren Geschwindigkeiten abbremsen, während auf der interstellaren Seite die Körner von wesentlich höheren Geschwindigkeiten abgebremst werden mussten. Die Aerogelzellen haben ein variierendes Dichteprofil: an der Oberfläche ist die Dichte geringer (5 mg/ml) und erhöht sich mit der Tiefe auf 30-50 mg/ml. Dieses Dichteprofil ist notwendig, da beim Einschlag der Körner auf das Auffangmedium ein hoher Druck entsteht, der umso geringer ist, je niedriger die Dichte im Moment des Auftreffens ist. Die Aerogelzellen für die Kometenpartikel haben drei Lagen mit unterschiedlichen Dichten, die Zellen für die interstellaren Körner haben zwei unterschiedliche Dichten (Tsou et al., 2003)....
New industries are recognized as new impetus to national wealth. At the same time, they are increasingly becoming geographically concentrated in some well defined areas. But current studies on the emergence of industrial clusters tend to analyze favorable driving factors. This dissertation takes the example of a Chinese endogenous industrial cluster, the traditional Chinese medicine (TCM) cluster at Tonghua, a small peripheral city in Northeastern China, to contribute to the theoretical understanding of the emergence of industrial cluster as a co-evolutionary process of organizations, institutions and firms, or, to put it more broadly, as economic evolution embedded in complex socio-economic contexts. The recent advance in evolutionary and co-evolutionary economics which considers the economy and economic landscape as dynamic process instead of equilibrium can be regarded as a part of broader and more intellectual turn of quest for history in social sciences. Although the principle of "history matters" is widely acknowledged, it tends to be reduced to a quite simple concept of "path dependence". However, path dependence cannot offer space for new path creation, except from an external shock. Accordingly, the role of human conscious action or Schumpeterian innovation should be added to path analysis through the concept of path creation. Furthermore, and more importantly, history should be understood as context, and historical context can be explored through the understanding of multi-paths and interaction among them over time. So path inter-dependence (co-evolution between paths) would be useful to better understand the complexity of real history. Since the industrial cluster is composed of interconnected firms and is also subject to changes in institution and technology, I will focus on the multi-way causal relationship between firm, institution and technology. The theorizing is not entirely new, but most of the theoretical and empirical discussions are at the national or industrial level, not regional or local one. A competitive cluster can be regarded as a co-evolutionary hotspot in which multiple populations actively interact and are interconnected. Co-evolution itself is a dynamic and evolutionary process. So I will adopt a dynamic and evolutionary view to examine co-evolutionary degree or co-evolutionary effects in the Tonghua pharmaceutical cluster through time. After a brief introduction which deals with the national institutional changes that are highly associated with new venture creation, entrepreneurship, and innovation, with registrations on drug and healthcare system, and with changes in market demand of China’s pharmaceutical industry and geographical distribution, I will collect evidences from three aspects based upon field survey and second hand data, i.e., the history of the enterprises, the origin of entrepreneurship, and the knowledge of evolution, linking their respective generative relationships through the genealogical method. In this volume, the evolution of the Tonghua pharmaceutical firm organization, the formation of local entrepreneurship, historical accumulation of knowledge, and particular knowledge of transfer among generations of firms will be discussed, then I will probe into co-adaption and co-evolution between local formal and informal institutions and organizations in Tonghua’s TCM industry. In addition, I will try to understand the co-evolutionary process at different geographical levels (namely, national and local). In summary, my main findings include the following several points. Firstly, in the course of the emergence of Tonghua’s pharmaceutical industry, local social networks and the traditional alliance between enterprises and government have played important roles. Secondly, the most important factor that influences the evolution of endogenous industrial clusters such as the Tonghua pharmaceutical industry in transitional countries is not the change in technology, but the change in fundamental national institutions. Thirdly, the success of the Tonghua pharmaceutical industry can be ascribed to the creation of multiple paths largely based on initial conditions, which implies that economic policy should have historical consciousness, namely, new economic innovation should make full use of both historical legacies and existing assets. Finally, it is co-adaption and co-selection of firm organization, institution, and technology that have jointly made Tonghua’s pharmaceutical industry become highly competitive, which means that whether one region can grasp new opportunities partially depends on its capabilities to coordinate a varity of development agents.
Trace elemental concentrations of bivalve shells content a wealthy of environmental and climatic information of the past, and therefore the studies of trace elemental distributions in bivalve shells gained increasing interest lately. However, after more than half century of research, most of the trace elemental variations are still not well understood and trace elemental proxies are far from being routinely applicable. This dissertation focuses on a better understanding of the trace elemental chemistry of Arctica islandica shells from Iceland, and paving the way for the application of the trace elemental proxies to reconstruct the environmental and climatic changes. Traits of trace elemental concentrations on A. islandica shells were explored and evaluated. Then based the geochemical traits of the shells, four non-environmental/climatic controlling is indentified. (1) Trace elemental concentrations of bivalve shells are effected by early diagenesis by the leach or exchange of elemental ions, especially in shell tip part, even with the protection of periostrucum; (2) The analytical methods also affect the results of trace elemental concentrations, especially for the element, such as Mg, which is highly enriched in organic matrices; (3) Shell organic matrices are found play a dominating role on the concentration of trace elements on A. islandica shells. Most trace elements only occurred in insoluble organic matrices (IOM), although others are only found in the carbonate fraction. IOM of A. islandica shells is significantly enriched in Mg, while Li and Na are more deplete in IOM, but enriched in shell carbonate. Ba is more or less even contented in IOM and shell carbonate. The concentrations of certain elements vary between primary layer and secondary layer; (4) The vital /physiological controlling on trace elemental distributions of bivalve shells is also confirmed. Six elemental (B, Na, Mg, Mn, Sr, and Ba) concentrations show significant correlation (exponential functions) with ontogenetic age and shell grow rates (logarithmic equations). It is worthy to remark that B, Mg, Sr and Ba concentrations are negatively correlated with shell growth rate, positive with ontogenetic age, while the concentrations of Na and Mn show the opposite trends. At last, all the controlling described above can be taken into account and corrected to extract the environmental and climatic signal by a kind of standardization. The derived six exponential functions of the high correlations between six trace elemental concentrations and ontogenetic year are applied to make the standardization of these element-Ca ratios. The gotten standardized indices are compared with the variations of environmental and climatic parameters in this region, and many correlations are found. Standardized indices of Sr/Ca ratios are strongly related to the sun spot number, autumn NAO, autumn Europe surface air temperature (SAT) and Arctic sea surface temperature anomaly (TA), and those of Mg/Ca ratios are strongly associated with Arctic TA, Europe SAT and Solar variation (irradiance). The variations of autumn Europe SAT demonstrated more similarity with standardized indices of B/Ca than other parameters. Except for the SAT index of Arctic, the standardized indices of Na/Ca showed no distinct relation to temperature. European precipitation and the Arctic sea level pressure index compared well the Na/Ca ratios of the shells, and so did the autumn NAO. Standardized indices of Mn/Ca were correlated with the number of hurricanes in the North Atlantic, Northern Europe SAT and sun spot number.