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This study investigates the postglacial sea-level history of eastern Cumberland Peninsula, a region of Baffin Island, Nunavut, where submerged terraces were documented in the 1970s. The elevation gradient of emerged postglacial marine-limit deltas and fiord-head moraines led Arthur Dyke to propose a conceptual model for continuous postglacial submergence of the eastern peninsula. Multibeam mapping over the past decade has revealed eight unequivocal submerged deltas at 19–45 m below present sea level (b.s.l.) and other relict shore-zone landforms (boulder barricade, spits, and sill platform) at 16–51 m b.s.l. Over a distance of 115 km from Qikiqtarjuaq to Cape Dyer, the submerged coastal features increase in depth toward the east, with a slope (0.36 m/km) less than that of the marine-limit shoreline previously documented (0.58–0.62 m/km). The submerged ice-proximal deltas, deglacial ice limits, and radiocarbon ages constrain the postglacial lowstand between 9.9 and 1.4 ka cal BP. The glacial-isostatic model ICE-7G_NA (VM7) computes a lowstand relative sea level at 8.0 ka, the depth of which increases eastward at 0.28 m/km. The difference between observed and model-derived lowstand depths ranges from 1 m in the west to 10 m in the east and the predicted tilt is significantly less than observed (p = 0.0008). The model results, emerging data on Holocene glacial readvances on eastern Baffin Island, and evidence for proglacial delta formation point to a Cockburn (9.5–8.2 ka) age for the lowstand, most likely later in this range. This study confirms the 1970s conceptual model of postglacial submergence in outer Cumberland Peninsula and provides field evidence for further refinement of glacial-isostatic adjustment models.

The Early Pleistocene is an epoch where wide environmental changes, driven by climate instabilities, were registered by multiple lines of evidence in different chronostratigraphic records, both continental and marine. Among these records, small mammals are one of the most reliable for understanding how faunal assemblages responded to the climate shifts. One of the key regions for this epoch in the European framework is the north-eastern Italian Peninsula, which was long considered as an ecotonal zone and crossroad between Central and Mediterranean Europe. In this region, Rivoli Veronese (Verona, north-eastern Italy), an Early Pleistocene site with a highly diversified assemblage, has always been considered one of the most important sites for the biochronology of the Italian Peninsula. Here we present the taxonomic study of the Early Pleistocene insectivores, bats, and rodents from this site, as well as the environmental and climatic reconstruction using the Taxonomical Habitat Index, the Habitat Weighting, and the Bioclimatic model. In the rich Rivoli Veronese assemblage, composed of 27 taxa, important biochronology markers, such as Mimomys pitymyoides, Mimomys tornensis, and Mimomys pliocaenicus were recognized. The earliest occurrences in Europe of Sorex praealpinus and Dinaromys genus were also documented as well as a new fossil mole species, Talpa sp. nov. Comparison with other European small mammal assemblages of the Early Pleistocene have allowed us to relate Rivoli Veronese to the early Late Villanyian Age. The persistence of Pliocene relicts, such as Rhagapodemus cf. frequens, and Pliopetaurista cf. pliocaenica, together with Early Pleistocene species is a remarkable feature of this site. This is also reflected in the environment which was still mainly forested but with spreading open areas and wetlands mainly in the form of water streams. The climate values shows that the conditions were similar to the current ones but the comparison with the near and recent Monte La Mesa assemblage, dated to Early Biharian (beginning of the Calabrian Stage), and the appearance of several taxa related to open landscapes show that a cooling and arid trend in climate was already settled in the region during the Gelasian.

From at least the Iron Age up to the Hellenistic period, the Etruscan culture flourished in a large portion of the Italian peninsula, extending from the Po delta and the eastern Alps in the north to Campania in the south. It was characterised by a magnificent and original artistic production that took its inspiration from aspects of the natural environment inserted into mythological contexts of various origins. In Etruscan art, birds occupied a significant place, and were often represented in wall paintings and craft objects. Species still occurring on the Italian mainland, such as swans, ducks, grouse, and partridges, as well as possibly exotic taxa, domestic forms (chickens and pigeons) and other unidentifiable birds were the subject of artistic inspiration. They were depicted not only in purely cult contexts, but also in the backgrounds of naturalistic landscapes.

Loess deposits are widely spread all over Eastern Europe, extending as far south as the Sea of Azov and the northern Black Sea. For many decades these regions have been noted for series of key sections. However, despite prolonged investigations, a lack of absolute dating and detailed lithological data has left many unresolved problems in the correlation of the regional stratigraphic schemes. In this study, integrated studies were undertaken on the loess-paleosol sequence exposed on the northern coast of the Taman Peninsula, separating the Sea of Azov from the Black Sea. The exposure in the coastal scarp near Cape Pekla was sampled in detail for standard lithological and stratigraphic analyses, and for the first time, detailed data on the sediments lithology and petromagnetic properties were obtained, as well as the first optically stimulated luminescence age estimates. The data lead us to conclude that the formation of continental series exposed in the Pekla section started at the beginning of the Middle Pleistocene. There are five well pronounced buried soil complexes (PS 1–5) exposed in the sequence, covering sedimentation from the Middle Pleistocene to the present day. We attribute two lower paleosols (PS 4 and PS 5) to two main warm intervals of the Middle Pleistocene – MIS 9 and MIS 13, and the Kamenka interglacial paleosol, correlated with MIS 7 from other parts of the Azov loess area, is represented in the Pekla section by a sand layer formed at the time of the marine transgression dated to interval 220–280 ka (MIS 7). The upper soil horizons (PS1, PS2 and PS3) developed between 20 and 220 ka. The Pekla section contains a considerable proportion of sand fraction – presumably, due to active eolian processes that developed in immediate vicinities of sources of the material. The paleosol characteristics and the structure of loess horizons in the Pekla subaerial series differ considerably from the well described loess-paleosol series of the Northern Azov Sea coasts. In all probability, this region of the Taman Peninsula belongs to a specific province located south of the North Azov loess-soil province.

El género Pisonia es primordialmente americano, se distribuye principalmente en regiones subtropicales y tropicales. En este trabajo se describe y documenta la nueva especie Pisonia calafia. Este taxon consiste de una relativamente pequeña población en la costa de la región de Los Cabos en la península de Baja California. La principal característica que diferencia a P. calafia del resto de las especies de este género es la carencia de sulcos y glándulas en el fruto. En adición a la descripción morfológica, se documenta la afinidad evolutiva del nuevo taxon con base en el análisis filogenético de la secuencia de nrITS. Las poblaciones conocidas consisten de unas pocas docenas de individuos, seriamente amenazados por el desarrollo de proyectos turísticos en la zona.

On the basis of surface air temperature (SAT) observations from the Great Wall Station located on the Antarctic Peninsula (AP) and ERA-Interim reanalysis data, the present manuscript investigates the role of atmospheric flow at intraseasonal and synoptic time scales in driving the temperature extremes over the AP during austral summer. Both warm and cold events can persist for multiple days and were maintained mainly by the advection of seasonal air temperature by intraseasonal winds. Synoptic winds can influence the temperature change around the peak time through their advection of seasonal temperature, thus determining the time of peak temperature anomalies. The generation of intraseasonal winds was closely associated with Rossby wave trains propagating along the polar front jet over the Atlantic sector of the Southern Ocean before the warm and cold events. The synoptic height anomalies before the warm events were also manifested as Rossby wave trains propagating along the polar front jet. However, synoptic Rossby wave trains were almost absent when the cold events occurred. Further analysis indicates that the weakened background flow during the cold events may have hindered the eastward travel of synoptic eddies. This study provides an important guidance for subseasonal to seasonal prediction on the AP.

The flat bark beetle fauna (Coleoptera: Cucujidae) has not been intensively studied in the Korean Peninsula; a few records of this insect family are known from the literature from this region. Based on the data collected from the iNaturalist citizen science database, local entomological fora and websites, as well as Facebook social media, new distributional data for Cucujidae are provided from the Korean Peninsula, including the first records of Cucujus haematodes haematodes from South Gyeongsang and North Chungcheong provinces and Pediacus japonicus from North Gyeongsang and South Jeolla provinces, all in South Korea. Moreover, critical analysis of the literature suggests excluding one species, Cucujus coccinatus, from the fauna of the entire Korean Peninsula as it was recorded based on misidentification with C. h. haematodes. The citizen scientific data made 74% of all known records of Cucujidae in the studied area, which clearly proves the importance of citizen science in studies focused on insect biodiversity, especially in the case of species characterized by at least medium body size. A country-level and province-level checklist and a diagnosis of Cucujidae species currently known from the Korean Peninsula are provided.

The coastal plain of West Sussex and south-east Hampshire preserves a succession of Pleistocene raised beaches, periglacial deposits, and estuarine channels. These incorporate numerous ‘erratics’ or ‘exotic’ rocks, here described as enigmatic rocks, and sarsen stones. The enigmatic rocks include large boulders of non-local igneous, metamorphic, and sedimentary rocks, which have attracted interest since the early 19th century. Many suggestions have been made regarding their origins, transport, and date of emplacement. More recently, it has been realised that these rocks may have important implications for understanding the Quaternary history of southern Britain and the palaeogeography of the English Channel region during the Pleistocene. This paper presents a literature review, supported by details of historic and extant boulders, distribution, and dimensions. In agreement with previous authors, it is concluded that the enigmatic rocks were likely transported within ice floes or icebergs, but further studies are required to identify possible sources. Suggestions have included northern Britain, Scotland, Scandinavia, Greenland and Laurentia. There are doubts concerning an adequate build-up of periglacial sea-ice to accept the historic consensus for a source in Brittany, the Cotentin Peninsula, and the Channel Islands. The date of emplacement is suggested to be MIS 13, but multiple phases of emplacement cannot be excluded. In contrast, the sarsen stones are considered to be relic of pre-MIS 7 periglacial erosion of weathered Lambeth Group in a regolith of Clay-with-flints formerly capping the local Chalk outcrop. Many questions remain unanswered, particularly regarding the enigmatic rocks, so aspects for future study are identified.

Interdecadal variations of the relationship between El Niño–Southern Oscillation (ENSO) and the Indo-China Peninsula (ICP) surface air temperature (SAT) in winter are investigated in the study. Generally, there exists a positive correlation between them during 1958–2015 because the ENSO-induced anomalous western North Pacific anticyclone (WNPAC) is conducive to pronounced temperature advection anomalies over the ICP. However, such correlation is unstable in time, having experienced a high-to-low transition around the mid-1970s and a recovery since the early 1990s. This oscillating relationship is owing to the anomalous WNPAC intensity in different decades. During the epoch of high correlation, the anomalous WNPAC and associated southwesterly winds over the ICP are stronger, which brings amounts of warm temperature advection and markedly heats the ICP. In contrast, a weaker WNPAC anomaly and insignificant ICP SAT anomalies are the circumstances for the epoch of low correlation. It is also found that substantial southwesterly wind anomalies over the ICP related to the anomalous WNPAC occur only when large sea surface temperature (SST) anomalies over the northwest Indian Ocean (NWIO) coincide with ENSO (viz., when the ENSO–NWIO SST connection is strong). The NWIO SST anomalies are capable of driving favorable atmospheric circulation that effectively alters ICP SAT and efficiently modulates the ENSO–ICP SAT correlation, which is further supported by numerical simulations utilizing the Community Atmospheric Model, version 4 (CAM4). This paper emphasizes the non-stationarity of the ENSO–ICP SAT relationship and also uncovers the underlying modulation factors, which has important implications for the seasonal prediction of the ICP temperature.

This study examines the long-term change in the threat of landfalling tropical cyclones (TCs) in East Asia over the period 1975–2020 with a focus on rapidly intensifying (RI) TCs. The increase in the annual number of RI-TCs over the western North Pacific and the northwestward shift of their genesis location lead to an increasing trend in the annual number of landfalling RI-TCs along the coast of East Asia. The annual power dissipation index (PDI), a measure of the destructive potential of RI-TCs at landfall, also shows a significant increasing trend due to increases in the annual frequency and mean landfall intensity of landfalling RI-TCs. The increase in mean landfall intensity is related to a higher lifetime maximum intensity (LMI) and the LMI location of the landfalling RI-TCs being closer to the coast. The increase in the annual PDI of East Asia is mainly associated with landfalling TCs in the southern (the Philippines, South China, and Vietnam) and northern parts (Japan and the Korean Peninsula) of East Asia due to long-term changes in vertical wind shear and TC heat potential. The former leads to a northwestward shift of favorable environments for TC genesis and intensification, resulting in the northwestward shift in the genesis, RI, and LMI locations of RI-TCs. The latter provides more heat energy from the ocean for TC intensification, increasing its chances to undergo RI.

The absence of large archaeological settlements in the Eastern Arabian Peninsula suggests that most of the recent wet periods occurring during climate oscillations in these areas were short-lived. However, a ∼ 2-by-3-km buried rectangular feature was discovered opportunistically in the southeast of the Qatar Peninsula while performing radar subsurface mapping of structural conduits for groundwater characterization. The feature is characterized by its unique contrasting patterns of surface and subsurface roughness as well as its organic-rich mixture of soils, as assessed from high-resolution radar and multispectral observations, respectively, and validated with GPR and EM subsurface probing. The above characteristics could be the only remaining evidence for a large primitive settlement due to the harsh erosive setting. To explore the natural or anthropogenic origin of this anomalous feature, we compare its dimensions, structural setting, roughness, and composition to similar formations in the Qatar Peninsula and other arid karst environments. Findings suggest that the feature is texturally and compositionally unique within the Qatar Peninsula, and is not reproduced in other arid karst terrains nor reproduced by the fracture patterns associated with the Qatar-South Fars Arch. We hypothesize that the feature is a karst depression modified by semi-stationary primitive human settlements ∼ 3640 BP or earlier based on radiocarbon dating of in-situ charcoal samples. Moreover, the organic-rich mixture of soil and the occurrence of several symmetrical features observed inside the perimeter suggest that landscaping, farming and irrigation activities could have occurred within the site, further suggesting that long-lasting wet conditions—with sufficient fresh water resources or reliance on karst aquifers—were able to sustain a relatively large primitive settlement not previously witnessed in the region’s archaeological record. Future improvements in the resolution and coverage of orbital L-band radar observations, as used above, can provide new insights into understanding prehistoric human occupation under fluctuating climatic conditions and groundwater dynamics in these hyper-arid regions.

In NW Anatolia, Eocene-Oligocene post-collisional magmatism is continued with long intervals. In this study, it is aimed to reveal the lithostratigraphic position and geochemical characteristics of volcanic rocks outcropping in the southeast of Lapseki (Çanakkale) in NW Anatolia. The magmatic rocks that compose the topic of this study can be classified lithostratigraphically into 6 different units in the region. In Eocene period, there are calc-alkaline Laledağgranodiorite and Beyçayır volcanics with andesite, dacite composition that are the intermediate character, and also Kızıldamvolcanics in characters of alkaline and basic character (basaltic trachyandesite, trachybasalt). Furthermore, in Oligocene period, the calc-alkaline volcanism starting with Dededağvolcanics with dacite and rhyolite composition in acidic-intermediate character has continued with Kırcalarvolcanics consisting of basalt and basaltic andesite, and Harmancık volcanics ranging from basalt to rhyolite. Çamyayla Pluton is intruded to Oligocene volcanics in the region. In this study, the geochemical data proved that magmatic units arein character of alkaline and calc-alkalinefor Eocene-Oligocene period. Alkaline lavas in the region are classified as high K and shoshonitic and calc-alkaline lavas have medium-high-K.

The study includes landslide movements that take place on Eocene and Middle-Upper Miocene aged the terrestrial and marine sedimentary rock units on the Canakkale basin in the Biga Peninsula. In this study, the active Ambaroba Landslide, Şevketiye and Adatepe Landslides located on the northern coasts of Biga Peninsula were investigated.The geological studies in the Ambaroba landslide have shown the integrity of the Bayramiç formation and the Şapcı volcanics in this area have shown their influence in the Miocene period.The sandstones in the Bayramiç formation are not very well paste and are yellow, dirty yellow and gray in color.The sliding surface units in the moving masses consist of non-hardening, very large blocky, pebbly and loose cement-bonded pebbles. In the Şevketiye and Adatepe Landslides, a sliding movement has occurred on the sandstone and conglomerate units with yellowish brown colors in the Fıçıtepe formation. The sandstones in these landslide areas are massive and well cemented. Conglomerates are weaker than sandstones and are fond of a gray-beige color that does not harden. Precipitation data and GPS measurements of the landslide areas were evaluated together with the lithological properties of the rocks.Loose sandstones and pebbles in the entire landslide areas studied can easily move due to seasonal precipitation.This movement was mostly seen in the Şevketiye landslide area and then in the Adatepe and Ambaroba areas, respectively. Although their effectiveness has decreased, the movements will continue, as the lithological features will not change in these areas. As a result, the measures specified in this study should be taken into account in order to eliminate the destructive effects of landslides.

Despite the wide popularity of the Crimean region, its scientific descriptions are full of gaps. In the Soviet period, the research was limited by the unspoken prohibitions on the study of social processes and by the absence of a strong scientific school. After the collapse of the USSR, the Crimean region was considered only in the works on social aspects of migration and on artificial transformations of the ethnic-confessional composition of the population. The change in the status of the Crimean Peninsula in 2014 made this region interesting for the Russian science: there are many recent articles on the features of the social-economic development of the peninsula, but a number of issues in the life of Crimea are still poorly understood. One of them is the migration on the peninsula: the historical ethnic migrations are sufficiently described but not the contemporary population movements. Historically, migration processes have played an important role in the social-economic development of Crimea. However, until recently, external migrations were the driver of this development, while since the beginning of the 21st century, migration movements within the peninsula have played this role, and their features should be taken into account in planning and financing the rural development. Rural areas of Crimea remain agrarian-overpopulated; therefore, it is necessary to identify areas promising for capital investment and areas that soon will be depopulated due to the lack of opportunities for human and social capital. The author considers the population exchange between urban and rural areas as an important factor for the demographic situation, and focuses on the reasons and features of the spatial mobility and migration of the Crimean population based on the analysis of statistical data and transport links between the city and the countryside.

We investigate long-term changes in winter rainfall patterns across the Arabian Peninsula (AP) through an analysis of the Climate Research Unit (CRU) gridded rainfall dataset, and long-term rainfall measurements collected at 39 stations distributed across the AP over the period 1951–2010. We reveal a long-term increase in winter rainfall of about 25–30% over the eastern AP and a long-term decrease of about 10–20% in the southern and northeastern AP. A partial correlation analysis suggests that canonical El Ninos are associated with significant negative winter rainfall anomalies in the southern and southwest AP during the 1951–1980 period. However, the extent of the El Nino-induced rainfall deficit decreased in subsequent decades. In fact, a significant above-average rainfall occurs in recent decades over Ethiopia, southwest Yemen and central AP during canonical El Ninos. Furthermore, positive phases of the Indian Ocean basin mode (IOBM), which lags the canonical ENSO signal by 3–4 months, are linked with significant below-average winter rainfall over the central and northern AP, but only until the 1970 s. We investigated the teleconnections between the variability of AP winter rainfall and various atmospheric parameters from the European Centre for Medium Range Weather Forecasting (ECMWF) twentieth century (ERA-20C) reanalysis. Notably, sub-tropical westerly jet (STJ) shifted southward and intensified over the AP during recent decades. This shift of the STJ favoured an increase in the frequent passage of transients, which contributed to increased winter rainfall over AP. These events anomalously strengthen the upper level westerlies during El Nino Modokis, adding to the recently-strengthened STJ over the AP, thereby further intensifying the transient activity. This large-scale background change likely weakened the impact of canonical El Nino and the IOBM events.

The Presque Isle Peninsula is a compound barrier-spit system perched atop a recessional moraine along Lake Erie’s southeastern coast. Its distal terminus, Gull Point, has grown to an extent of around 0.6 km2 since the early 1900s, promoted by beach nourishment along the peninsula proper and later influenced by a change in local hydrodynamic regime following breakwater installation near the attachment point. This coastal setting has set the stage for an analysis of ridge landform- and vegetation-succession dynamics using historical aerial images, a series of high-resolution LiDAR datasets, transect/quadrat surveys of vegetation, and increment core dates of tree cohorts on dune ridges separated by swales and lagoons. The general evolutionary model is one of punctuated landform growth to the east by lateral accretion, interspersed with erosional events and ridge recurving towards the backbarrier. Eastern cottonwood (Populus deltoides), with its minimally provisioned wind- and water-dispersed seeds, colonizes the margins of newly deposited sand ridges as discrete cohorts, and dominates the tree stratum of Gull Point. These cohorts are increasingly mature moving from distal to proximal zones, and consistently reflect the temporal sequence of ridge morphology. Vegetation communities, representing a primary successional chronosequence, are delineated into four phases extending back to the 1950s, which are roughly demarcated by erosional ridgelines of topographic prominence, revealing a tight coupling of lake-level trends, geomorphology, and vegetation dynamics. This provides coastal researchers with a means of understanding landform-age relationships across structurally complex strand areas for which age-relationships cannot be ascertained by aerial photographic records alone.

Coastal dunes are prominent features along the Lake Michigan shoreline, especially along Michigan’s Lower Peninsula. Numerous studies in recent years have reconstructed the geomorphic history of these dune systems, from their initial formation in the mid-Holocene to about 300 years ago. These studies have suggested linkages between past dune behavior and climatic variability and fluctuating lake levels. Less is known, however, about how these dune systems change on shorter-temporal scales in the modern era and the potential drivers of that change. Using repeat photography, this paper attempts to demonstrate how the coastal dunes of Lake Michigan’s eastern shore have changed since the 19th century. We collected hundreds of photographs of these dunes, taken between the years 1885 and 2018, from archives and citizen scientists. In the spring and summer of 2019, we took ∼70 new photographs replicating the original images. The changes between coastal dune conditions in the original photographs and in the 2019 photographs show a general expansion of vegetation across formerly barren and active surfaces along the entire shoreline. Although human development has also played a role in reshaping the coastal dune systems, the most pronounced difference between historical and current dune conditions where repeat photography was conducted is the expansion of vegetation – grasses, shrubs, and even trees. Here, we present the 20 photograph pairs most representative of these trends, explore these changes, and discuss the likely causes, including the increase in precipitation in Michigan in the past ∼80 years.

The drywood termite Kalotermitidae Froggatt, represented by Glyptotermes nakajimai Morimoto, is identified for the first time in Korea. They were collected in Yeoseo-do Island, the southern part of the Korean peninsula. A key to the termite species in Korea, habitus photographs of all castes, ecological information, and illustrations of diagnostic characters are provided.

Understanding the relationship between migratory performance and fitness is crucial for predicting population dynamics of migratory species. In this study, we used geolocators to explore migration performance (speed and duration of migratory movements, migratory timings) and its association with breeding phenology and productivity in an Afro-Palearctic insectivore, the European bee-eater (Merops apiaster), breeding in Iberian Peninsula. Bee-eaters migrated at higher travel speeds and had shorter travel duration in spring compared to autumn. Individuals that departed earlier or spent fewer days in-flight arrived earlier to the breeding areas. Our results show overall positive, but year-specific, linkages between arrival and laying dates. In one year, laying was earlier and productivity was higher, remaining constant throughout the season, while in the subsequent year productivity was lower and, importantly, declined with laying date. These results suggest that arriving earlier can be advantageous for bee-eaters, as in years when breeding conditions are favourable, early and late breeders produce high and similar number of fledglings, but when conditions are unfavourable only early breeders experience high productivity levels.

There exists a need to document details related to the spatiotemporal climatology of precipitation over the Arabian Peninsula (Arabia) based on a sound assessment. Areal precipitation was calculated for Arabia, subtropical Arabia (STA), and tropical Arabia (TA) using a weighting scheme to adjust for latitudinal changes in grid-cell areas and extract statistics that have geographical/spatial interpretation based on a quality-controlled spatially-distributed precipitation dataset (1980–2019). Areal annual precipitation mean over Arabia (STA/TA) is 88.61 mm (85.72/92.79). While boreal winter and spring seasons are the wet seasons over Arabia (29, 40%) and STA (36, 40%), boreal spring and summer are the wet seasons over TA (41, 25%). Only 25% of Arabia (STA/TA) receives more than 110.73 (108.48/113.73) mm of precipitation annually. Spatiotemporal trends were explored using the Mann–Kendall test, applied to trend free pre-whitened data, and the Theil-Sen estimator. Average areal precipitation over Arabia and STA is decreasing during the boreal winter and spring seasons at varying rates. On the other hand, boreal summer and fall precipitation is increasing over Arabia, STA, and TA with only that of TA summer being statistically significant. An elongated region extending from southwest to northeast has a statistically significant negative trend in annual, spring, and winter precipitation. The southern part of Arabia is dominated by positive trends in annual, summer, and fall precipitation with only isolated areas being statistically significant. The statistically significant decreasing trend in wet season precipitation over Arabia calls for more conservative water resource management strategies and bold adaptation measures.