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Marine molluscs are exceptional in Cretaceous ambers. Palaeoellobium decampsi gen. nov., sp. nov. is the first gastropod ever preserved in French uppermost Albian-lowermost Cenomanian opaque amber. It belongs to the Ellobiidae that are distributed in the Cenozoic supralittoral zones in close vicinity of the mangroves. It has been discovered by non-destructive X-ray phase-contrast imaging. The forest of conifers that produced the amber embedding this gastropod did not form its habitat, and it may have been transported to the foreshore detritus. Palaeoellobium decampsi contributes to the understanding of the ellobiid early adaptive radiation known by few taxa, compared with the significant Cenozoic diversification.
This perspective article invites readers to (re)imagine research as a means of practicing right relations with the places we inhabit and descend from. We anchor our work in a Kanaka Hawaiʻi, a Native Hawaiian cosmogeny and epistemology, one that recognizes all life as kin. We begin with the central question, “Where have the sand turtles gone?” to explore how a Kanaka Hawaiʻi-informed perspective, grounded in the genealogical creation chant, ke Kumulipo, can guide plastics research in Hawaiʻi. We elaborate this perspective through a moʻolelo, a story of a collaboration between a Kanaka Hawaiʻi cultural practitioner and a French and Swedish plastics researcher along the shores of Kapua, Waimānalo. By tracing the transformation of a conventional scientific study, we aim to grow entry points for research that is accountable to the place and the genealogical descendants of those specific lands, who have inherited the privilege and responsibility to steward them. We conclude by discussing how this perspective might offer critical insights for global environmental policy, such as the UN Plastic Treaty, urging a shift from treating Indigenous Peoples as stakeholders to honoring them as rights-holders. Ultimately, this work is a call to research in ways that honor the original peoples of the places where we are blessed to live, work, and research, particularly in ways that amplify the knowledge traditions and lifeways birthed from those specific lands. We write this piece for and with Waimānalo as a living, reciprocal co-author. We hope the experiences shared here return to and strengthen those places and people.
Fossils and more recent remains of dead organisms serve as natural archives of Earth’s recent and ancient history. It is often the case that small or fragmented specimens, especially microvertebrate bones, go unstudied. Accurate identification of such remains to a specific taxonomic level can help address a wide range of questions spanning paleontology, paleoecology, zooarchaeology, ecology, conservation science, forensics, and biogeography. Geometric morphometrics demonstrates significant potential for identifying fragmented lizard fossils to at least the family level based on shape differentiation. Our proof-of-concept study using lizard maxillae of extant species within the Pacific Northwest, USA, accurately identified fragmented maxillae with as few as six comparative specimens per genus. These findings establish a framework for addressing taxonomic challenges in fragmented bone specimen identification for taxa whose curated comparative specimens are small in number and unequal in representation.
A new species of Pseudocorax (Lamniformes, Pseudocoracidae), Pseudocorax heteroserratus n. sp., is described from the upper Maastrichtian phosphates of Morocco. This novel taxon is recognized by a large sample of isolated teeth collected from the upper Couche III layer at the Sidi Chennane quarry in the Oulad Abdoun Basin, Khouribga Province, Morocco. P. heteroserratus is differentiated from other Pseudocorax species by bearing a mesiodistally elongated tooth base, broad crown, and highly variable serrations. The variability in number and extent of serrations along the carinae ranges from completely absent to fully serrated and finely to coarsely serrated, raising speculation on broader Pseudocorax phylogenetics and as to whether the genesis of serrations within Pseudocorax occurred in a singular progressive event or rather from two distinct events. The morphological variability within the new species highlights the importance of large sample sizes in selachian odontological studies using isolated teeth.
The modulation of drag through dispersed phases in wall turbulence has been a longstanding focus. This study examines the effects of particle Stokes number ($\textit{St}$) and Froude number ($\textit{Fr}$) on drag modulation in turbulent Taylor–Couette (TC) flow, using a two-way coupled Eulerian–Lagrangian approach with Reynolds number ${\textit{Re}}_i = r_i \omega _i d/\nu$ fixed at 3500. Here, $\textit{St}$ characterises particle inertia relative to the flow time scale, while $\textit{Fr}$ describes the balance between gravitational settling and inertial forces in the flow. For light particles (small $\textit{St}$), drag reduction is observed in the TC system, exhibiting a non-monotonic dependence on $\textit{Fr}$. Specifically, drag reduction initially increases and then decreases with stronger influence of gravitational settling (characterised by inverse of $\textit{Fr}$), indicating the presence of an optimal $\textit{Fr}$ for maximum drag reduction. For heavy particles, a similar non-monotonic trend can also be observed, but significant drag enhancement results at large $\textit{Fr}^{-1}$. We further elucidate the role of settling particles in modulating the flow structure in TC flow by decomposing the advective flux into contributions from coherent Taylor vortices and background turbulent fluctuations. At moderate effects of particle inertia and gravitational settling, particles suppress the coherence of Taylor vortices which markedly reduces angular velocity transport and thus leads to drag reduction. However, with increasing influence of particle inertia and gravitational settling, the flow undergoes abrupt change. Rapidly settling particles disrupt the Taylor vortices, shifting the bulk flow from a vortex-dominated regime to one characterised by particle-induced turbulence. With the dominance of particle-induced turbulence, velocity plumes – initially transported by small-scale Görtler vortices near the cylinder wall and large-scale Taylor vortices in the bulk region – are instead carried into the bulk by turbulent fluctuations driven by the settling particles. As a result, angular velocity transport is enhanced, leading to enhanced drag. These findings offer new insights for tailoring drag in industrial applications involving dispersed phases in wall-bounded turbulent flows.
Antarctic ice-free coastal environments, like the Vestfold Hills (East Antarctica), are shaped by a complex interplay of physical processes. This study synthesizes new data and existing research from the Vestfold Hills across marine, terrestrial and cryosphere science, meteorology, geomorphology, coastal oceanography and hydrology to explore interconnected processes ranging from icescape morphology and sediment transport to ocean-floor scouring and ocean-atmosphere interactions. Coastal landforms and habitats result from the interaction of marine dynamics with the aeolian and fluvial transport of glacially derived sediments and geomorphic features. Rocky shorelines dominate the region, and extensive fjords are prominent coastal features, whereas intertidal sediments and beaches are scarce. The marine environment is characterized by slow currents, low-energy waves, annually variable land-fast ice, irregular sedimentation rates and a geomorphologically complex shoreline. Aeolian and fluvial sediment deposition into coastal waters and onto sea ice can significantly impact local ecological and physical processes. Human activity further modifies these dynamics. Ice-free coastal areas such as the Vestfold Hills are predicted to experience substantial environmental shifts due to climate change. Wind speeds, temperature and precipitation are increasing in the Vestfold Hills. Retreating grounded ice sheets are likely to expand this coastal area and increase meltwater and sediment inputs into nearshore marine systems. Concurrently, changes in sea-ice extent, thickness and/or duration may profoundly alter the structure and function of this coastal environment.
Scientists have developed complex computer models to produce climate simulations. The models produce maps that are depictions of how the world of doubled CO2 in the computer differs from the present-day world. One thing that climate models must do skillfully to get the doubled-CO2 climate right is to simulate the present climate realistically. For example, the effect of CO2 in the polar regions is largely dominated by whether there is ice and snow to melt. If there is, then we get a feedback effect, because when it melts, the darker, newly exposed surface absorbs more sunlight. The main challenge of climate modeling is getting the feedbacks right. At present, we cannot blindly rely on the results of climate models, because we are not sure about the extent or magnitude of the feedbacks. In models, the virtual world warms in response to increasing atmospheric carbon dioxide concentrations. Different models with different treatments of important feedback mechanisms give somewhat different magnitudes for the warming.
Any rational response to climate change involves first knowing what the facts and evidence are. That is the province of science. For example, how do we know the ocean is warming? We now measure the increase in ocean heat content from an array of about 4,000 autonomous floats deployed throughout the world ocean under an international program called Argo. They are programmed to rise and sink by changing their volume. This is accomplished by pumping fluid into or out of a bladder on the float. The floats store the measurements, and then, when they are on the surface, they locate by GPS and transmit the stored data via satellites to scientists. The Argo floats have revolutionized our ability to observe the oceans. Argo data are available to everyone for free in near real time. The science is never complete. There is always more to learn. But the science that we have now is already good enough to help us make wise decisions. “Everybody is entitled to his own opinions, but not to his own facts.” Sound science can inform wise policy.
Climate change is an important existential issue for our time. This book is an anthology of readings about climate change science. The rationale for writing this book is that some universities are now beginning to require all undergraduate students to take an approved climate change course. The book is for students who may lack strong mathematical backgrounds or may not have taken some science courses. It also for the general reader who wants to understand climate change science. The book has no equations and no technical jargon and no complex charts or graphs. Anyone who can read a newspaper can read this book. The book explains how the climate change issue has developed over many decades, how the science has progressed, how diplomacy has proven unable to find a means of limiting global emissions of heat-trapping substances such as carbon dioxide created by burning fossil fuels (coal, oil, and natural gas), and how the forecast of the resulting climate change has become more worrisome.
The urgency of acting to limit climate change has nothing to do with politics or economics. Instead, it arises directly from the physics and chemistry of the climate system. Carbon dioxide, once it is added to the atmosphere, will remain there a long time. Some of it will remain in the atmosphere for centuries until natural processes remove it. Thus, it will be there essentially forever, if we think in terms of the implications on human time scales. The only known way to prevent atmospheric carbon dioxide amounts from increasing further is simply to cease emitting carbon dioxide into the atmosphere. That is why acting swiftly to make large reductions in global emissions, in order to limit climate change, is urgent. Yet very little significant progress has occurred toward actually making the large cuts in global emissions of heat-trapping gases that would be needed to stabilize climate. Without drastic and rapid cuts in emissions, our children and their descendants, and ultimately all living things, will be faced with the consequences of more severe climate disruption.
The threat of climate change was already becoming clear to some climate scientists by the 1970s. However, the scientific community had not yet brought the details of this threat to the attention of the world. A towering figure in climate science, Stephen H. Schneider, 65, died after suffering a pulmonary embolism on July 19, 2010, while flying to London from a conference in Stockholm. The loss of Schneider, a professor at Stanford University, deprives the world of both an outstanding researcher and a gifted science communicator. Although his eloquent voice has now been silenced, his powerful influence on us all is indelible, and the example of the life he led will continue to be an inspiration. The effort at climate change science communication is not something novel and recent, but it has occupied many of us climate scientists for at least half a century. I also want to emphasize that climate change science communication needs to continue, because the world has not yet acted forcefully and effectively enough to limit climate change to an amount that nations of the world have agreed on.
Hillel, some 2,000 years ago, gave a brief explanation of the five books of the Torah. These books are known to Christians as the first five books of the Old Testament. Hillel said, “Treat others as you would wish them to treat you. That is the entire Torah. The rest is commentary. Now go and study.” I am certainly not Hillel, science is obviously not religion, and the IPCC reports are not the Torah. But I think the essence of the most recent IPCC report can be summarized in 12 succinct points. Here they are: It is warming. It is us. It has not stopped. The heat is mainly in the sea. Sea level is rising. Ice is shrinking. CO2 makes oceans more acidic. CO2 in the air is up 50% since the 1800s. It is now the highest in millions of years. Cumulative emissions set the warming. Reducing emissions limits the warming. Climate change will last for centuries.
Based on the generalised Saint-Venant equations for granular flow on an inclined chute, we show how to generate solitary waves from localised perturbations at the inlet. Such perturbations usually give rise to a group of roll waves, but by choosing the system parameters appropriately, the formation of all but the first wave can be suppressed, thus turning this first one into a solitary wave. This calls for a highly diffusive flow, which is realised for inclination angles close to the minimal angle required to keep the granular material flowing.
Chapter 4 provides an environmental interpretation of Kant’s aesthetic and teleological theory as developed in the Critique of the Power of Judgment. To put Kant’s insights in dialogue with new contributions in climate aesthetics, I begin with Kant’s theory of the sublime. I claim that Kant’s account of the dynamical sublime has important moral and political relevance for climate philosophy despite its human-centered focus. Next, I look into Kant’s account of natural beauty, which I suggest justifies duties against environmental degradation. I also touch on Kant’s duties to love nature’s harmony and purposes in light of ecological stewardship. The chapter concludes with a look into Kantian teleology from the Critique of Judgment. I propose that teleological judgment can be used to motivate protection of non-beautiful aspects of ecosystems, especially in light of climate-related biodiversity loss.
I urge every climate change science communicator (including anyone speaking to family and friends and colleagues) to heed these warnings. Do not follow the example of the scientist who communicates all the details and background first and then announces the results and conclusions at the end. In journalism, this sin is called “burying the lead.” Avoid metric units when speaking to Americans. Avoid unfamiliar terms that always have familiar substitutes. Rather than “anthropogenic,” you could and should say “human caused.” Do not use jargon. Try to compose messages that are simple and memorable, to repeat them often, and to partner with trusted messengers. Use metaphors and other vivid imagery. If climate change is important to you, do not speak or write about it in dry and unemotional language that conveys boredom and resignation. Instead, let your passion show. Profit from opportunities to learn from expert communicators and to get useful feedback. Nobody is born knowing how to ski or drive a car. Like these skills, communication skills can be taught, developed, practiced, and improved.