A Review of the Morphology, Physical Processes and Deposits of Modern Straits

This study reviews the morphology, hydrodynamics and sedimentology of 33 modern straits, including examples from diverse tectonic and climatic settings. Strait morphology ranges from short, simple straits to long, tortuous passages many 100s of kilometers long; depths range from 10 m to >1 km. The morphological building block of strait sedimentation is a constriction flanked by open basins; a single strait can contain one or several of these. Currents accelerate through the constrictions and decelerate in the basins, leading to a spatial alternation of high- and low-energy conditions. Currents in a strait can be classified as either ‘persistent’ (oceanic currents or density-driven circulation) or ‘intermittent’ (tidally or meteorologically generated currents). Constrictions tend to be bedload partings, with the development of transport paths that diverge outward. Deposition occurs where the flow decelerates, generating paired subaqueous ‘constriction-related deltas’ that can be of unequal size. Cross-bedding predominates in high-energy settings; muddy sediment waves and contourite drifts are present in some straits. In shallow straits that were exposed during the sea-level lowstand, strait deposits typically occur near or at the maximum flooding surface, and can overlie estuarine and fluvial deposits. The most energetic deposits need not occur at the time of maximum inundation.Supplementary material at https://doi.org/10.6084/m9.figshare.c.5746061

Evidence for a Recent Formation of the Isthmus of Panama 0.6 Mya

The exact age of the final formation of the Isthmus of Panama is a critical reference point for oceanographic, climatic, biogeographic, and evolutionary hypotheses. Geotectonic evidence suggests that the isthmus was completed between 12 Mya and 3 Mya, and an age of 3–4 Mya has been used as a benchmark in hundreds of studies over the past 30 years. Phylogeographic data indicate the existence of marine connections across the isthmus much more recently, however. I reconsider the available geotectonic, biostratigraphic, oceanographic, and paleoclimatic data and show that multiple lines of indirect evidence suggest that four transisthmian seaways may have persisted until as recently as the onset of the Middle Pleistocene (~ 0.6 Mya). Subduction of the Cocos Plate beneath one transisthmian seaway (the only seaway featuring a deep sill) caused rapid tectonic shoaling and reorganisation of oceanic currents, which coincided with a major glacioeustatic sea level fall ~ 950–917 Mya that led to a temporary closing of the Bering Strait. This resulted in unusual and contrasting climate phenomena, including the “900-Kyr (cold) event” and the “greening” of South Greenland during the MIS 22 glacial maximum. The concurrence of the final formation of the Isthmus of Panama with the mid-Pleistocene Transition of glacial/interglacial periodicity suggests a tight relationship between these events.

Echofacies interpretation of Pleistocene to Holocene contourites on the Demerara Plateau and abyssal plain

Off French Guiana and Suriname, North Atlantic Deep Water and Antarctic Bottom Water oceanic currents contour the Demerara marginal plateau, which promotes the formation of contourites. We have studied these contourites thanks to a new compilation of high-resolution subbottom profiles calibrated by sedimentary cores. The echofacies and isopach maps that we constructed highlight a sedimentary distribution parallel to the isobaths. The presence of moats along the slope is confirmed by the observation of parallel, elongated, sedimentary depleted zones and echofacies strongly affected by diffraction hyperbola and transparent echofacies. We interpret these features to be related to eroded slopes and mass-transport deposits. In contrast, the sedimentary drifts that we mapped are characterized by elongated and thick slope-parallel depocenters displaying bedded echofacies with wave-like bedforms. According to our interpretation, they result from interactions between the currents and the seafloor. Seismic wipeouts frequently affect those drifts, possibly resulting from high water or organic contents.

Ocean Currents Drove Genetic Structure of Seven Dominant Mangrove Species Along the Coastlines of Southern China

Mangrove forest ecosystems, which provide important ecological services for marine environments and human activities, are being destroyed worldwide at an alarming rate. The objective of our study was to use molecular data and analytical techniques to separate the effects of historical and contemporary processes on the distribution of mangroves and patterns of population genetic differentiation. Seven mangrove species (Acanthus ilicifolius, Aegiceras corniculatum, Avicennia marina, Bruguiera gymnorrhiza, Kandelia obovata, Lumnitzera racemosa, and Rhizophora stylosa), which are predominant along the coastlines of South China, were genotyped at nuclear (nSSR) and chloroplast (cpSSR) microsatellite markers. We estimated historical and contemporary gene flow, the genetic diversity and population structure of seven mangrove species in China. All of these seven species exhibited few haplotypes, low levels of genetic diversity (HE = 0.160–0.361, with the exception of K. obovata) and high levels of inbreeding (FIS = 0.104–0.637), which may be due to their marginal geographical distribution, human-driven and natural stressors on habitat loss and fragmentation. The distribution patterns of haplotypes and population genetic structures of seven mangrove species in China suggest historical connectivity between populations over a large geographic area. In contrast, significant genetic differentiation [FST = 0.165–0.629 (nSSR); GST = 0.173–0.923 (cpSSR)] indicates that populations of mangroves are isolated from one another with low levels of contemporary gene flow among populations. Our results suggest that populations of mangroves were historically more widely inter-connected and have recently been isolated, likely through a combination of ocean currents and human activities. In addition, genetic admixture in Beibu Gulf populations and populations surrounding Hainan Island and southern mainland China were attributed to asymmetric gene flow along prevailing oceanic currents in China in historical times. Even ocean currents promote genetic exchanges among mangrove populations, which are still unable to offset the effects of natural and anthropogenic fragmentation. The recent isolation and lack of gene flow among populations of mangroves may affect their long-term survival along the coastlines of South China. Our study enhances the understanding of oceanic currents contributing to population connectivity, and the effects of anthropogenic and natural habitat fragmentation on mangroves, thereby informing future conservation efforts and seascape genetics toward mangroves.

Oceans as the Paradigm of History

The temporality of historical flows can be understood through the paradigm of oceanic circulations of water. Historical processes are not linear and tunneled but circulatory and global, like oceanic currents. The argument of distributed agency deriving from the ‘ontological turn’ dovetails with the oceanic paradigm of circulatory histories. The latter allows us to grasp modes of both natural and historical inter-temporal communication through the medium of the natural and built environment. Yet the inclination in these new studies to deny any particular privilege to human will or design risks neglecting the changing role of human agency. Analytically I distinguish historiographical time from historical time. Historiographical time may be seen as the purposive capture of historical processes for various goals whereas historical time is more continuous with natural flows. More than origins and causes, the paradigm emphasizes the ramifying con-sequences of purposive actions. The gap in our understanding of the two temporalities has had a devastating impact on the planet.