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The scarcity of high-resolution empirical data directly tracking diversity over time limits our understanding of speciation and extinction dynamics and the drivers of rate changes. Here, we analyze a continuous species-level fossil record of endemic diatoms from ancient Lake Ohrid, along with environmental and climate indicator time series since lake formation 1.36 million years (Ma) ago. We show that speciation and extinction rates nearly simultaneously decreased in the environmentally dynamic phase after ecosystem formation and stabilized after deep-water conditions established in Lake Ohrid. As the lake deepens, we also see a switch in the macroevolutionary trade-off, resulting in a transition from a volatile assemblage of short-lived endemic species to a stable community of long-lived species. Our results emphasize the importance of the interplay between environmental/climate change, ecosystem stability, and environmental limits to diversity for diversification processes. The study also provides a new understanding of evolutionary dynamics in long-lived ecosystems.

Introduction: The establishment of venous access is one of the driving factors for complications during implantation of pacemakers and defibrillators (cardiac implantable electronic devices [CIED]). Recently, a novel approach of accessing the cephalic vein for CIED by cephalic vein puncture (CVP) using a modified Seldinger technique has been described, promising high success rates and simplified handling with steeper learning curves. In this single‐center registry, we analyzed the safety and efficiency of CVP to SVP access after defining CVP as the primary access route in our center. Methods: A total of 229 consecutive patients receiving a CIED were included in the registry. Sixty‐one patients were implanted by primary or bail‐out SVP; 168 patients received primary cephalic preparation and CVP was performed when possible, using a hydrophilic transradial sheath. Results: Implantation of at least one lead via CVP was successful in 151 of 168 patients (90%), and implantation of all leads was possible in 122 of 168 patients (72.6%). Total implantation times and fluoroscopy times and doses did not differ between CVP and SVP implantations. Pneumothorax occurred in 0/122 patients implanted via CVP alone, but 8/107 (7.5%) patients received at least one lead via SVP. Conclusion: Our data confirms high success rates of the CVP for CIED implantation. Moreover, this method can be used without significantly prolonging the total procedure time or applying fluoroscopy dose compared to the highly efficient SVP while showing lower overall complication rates. [ABSTRACT FROM AUTHOR]

The element mercury (Hg) is a key pollutant, and much insight has been gained by studying the present-day Hg cycle. However, many important processes within this cycle operate on timescales responsive to centennial- to millennial-scale environmental variability, highlighting the importance of also investigating the longer-term Hg records in sedimentary archives. To this end, we here explore the timing, magnitude, and expression of Hg signals retained in sediments over the past ∼ 90 kyr from two lakes, linked by a subterranean karst system: Lake Prespa (Greece, North Macedonia, and Albania) and Lake Ohrid (North Macedonia and Albania). Results suggest that Hg fluctuations are largely independent of variability in common host phases in each lake, and the recorded sedimentary Hg signals show distinct differences first during the Late Pleistocene (Marine Isotope Stages 2–5). The Hg signals in Lake Prespa sediments highlight an abrupt, short-lived peak in Hg accumulation coinciding with local deglaciation. In contrast, Lake Ohrid shows a broader interval with enhanced Hg accumulation and, superimposed, a series of low-amplitude oscillations in Hg concentration peaking during the Last Glacial Maximum, which may result from elevated clastic inputs. Divergent Hg signals are also recorded during the Early and Middle Holocene (Marine Isotope Stage 1). Here, Lake Prespa sediments show a series of large Hg peaks, while Lake Ohrid sediments show a progression to lower Hg values. Since ∼ 3 ka , anthropogenic influences overwhelm local fluxes in both lakes. The lack of coherence in Hg accumulation between the two lakes suggests that, in the absence of an exceptional perturbation, local differences in sediment composition, lake structure, Hg sources, and water balance all influence the local Hg cycle and determine the extent to which Hg signals reflect local- or global-scale environmental changes. [ABSTRACT FROM AUTHOR]

Mediterranean climates are characterized by strong seasonal contrasts between dry summers and wet winters. Changes in winter rainfall are critical for regional socioeconomic development, but are difficult to simulate accurately.sup.1 and reconstruct on Quaternary timescales. This is partly because regional hydroclimate records that cover multiple glacial-interglacial cycles.sup.2,3 with different orbital geometries, global ice volume and atmospheric greenhouse gas concentrations are scarce. Moreover, the underlying mechanisms of change and their persistence remain unexplored. Here we show that, over the past 1.36 million years, wet winters in the northcentral Mediterranean tend to occur with high contrasts in local, seasonal insolation and a vigorous African summer monsoon. Our proxy time series from Lake Ohrid on the Balkan Peninsula, together with a 784,000-year transient climate model hindcast, suggest that increased sea surface temperatures amplify local cyclone development and refuel North Atlantic low-pressure systems that enter the Mediterranean during phases of low continental ice volume and high concentrations of atmospheric greenhouse gases. A comparison with modern reanalysis data shows that current drivers of the amount of rainfall in the Mediterranean share some similarities to those that drive the reconstructed increases in precipitation. Our data cover multiple insolation maxima and are therefore an important benchmark for testing climate model performance. Comparisons between past regional drivers of precipitation extremes found time series data from Lake Ohrid and modern climate models of the Mediterranean may help to reduce simulation uncertainties in predictions of the Mediterranean climate., Author(s): Bernd Wagner [sup.1] , Hendrik Vogel [sup.2] , Alexander Francke [sup.1] [sup.3] , Tobias Friedrich [sup.4] , Timme Donders [sup.5] , Jack H. Lacey [sup.6] , Melanie J. Leng [...]

Perovskite oxides of the general formula ABO3−δ, with A and B being metal cations, present themselves in various crystal structures that originate from a distorted ideal cubic perovskite. Understanding how composition, temperature, atmosphere and reduction extent of these non-stoichiometric redox materials induce structural changes on an atomic, as well as macroscopic, level is crucial to transfer newly developed materials to industrial scale applications in the redox-based energy conversion sector. Herein, Ca1−xSrxMnO3−δ (x ∈ [0,0.2]) and its micro- and macroscopic structural changes at elevated temperatures and varying oxygen partial pressure are analyzed by means of in situ high temperature XRD, DSC and dilatometry. Results are expanded by room temperature XRD of compositions with higher Sr-content up to x = 0.4. By adjusting the Sr-content, the formed crystal structure can be governed and thermal expansion can be impacted beneficially in the context of future applications utilizing monolithic structures. Phase transitions from orthorhombic to cubic were found to shift from 900 °C to 830 °C under air and to even lower temperatures under 1% O2 atmosphere. Small amounts of Sr-content (5–10%) stabilize the macroscopic structural integrity by improving the reversibility of the cyclic thermal expansion and contraction in a 1% O2 atmosphere. However, at Sr-contents of 20% an increased irreversible residual expansion within each thermal cycle becomes apparent and shows that such improvements do not follow a linear dependency with Sr-content, but most benefits in this context can be found at Sr-contents below 20%. The results demonstrate the sensitivity of such materials micro- and macroscopic characteristics to composition. In the context of utilization of monolithic structures, fabricated entirely from Ca1−xSrxMnO3−δ, in thermochemical or thermoelectric applications, the results have considerable significance as minor A-site Sr-substitution can substantially improve macroscopic stability of monolithic structures over multiple thermal cycles. Besides the often solely regarded thermodynamic characteristic, this work demonstrates the importance to consider the impact of composition on structural behavior in materials design processes including perovskites for thermochemical applications. [ABSTRACT FROM AUTHOR]