The terrestrial and marine biotypes of Madagascar are critical priorities for conservation, with almost unparalleled levels of endemism, species diversity and human threat for a land area of its size. Field inventories and molecular-based research conducted from the mid 1980s to present have greatly expanded knowledge of the country's biota, for some groups with nearly exponential growth in measures of species diversity. I provide updated measures of estimated species diversity between a book with 289 contributors, published in 2003 (The Natural History of Madagascar), and a full-scale update with 539 contributors, published in 2022 (The New Natural History of Madagascar). I compare biodiversity information presented in the new book with data from the earlier book, providing insight into scientific advancements, and revised estimates of species richness and endemism of a range of taxonomic groups.

Precise radiocarbon (14C) dating of sedimentary sequences is important for developing robust chronologies of environmental change, but sampling of suitable components can be challenging in highly dynamic landscapes. Here we investigate radiocarbon determinations of different peat size fractions from six peat sites, representing a range of geomorphological contexts on the South Atlantic subantarctic islands of the Falklands and South Georgia. To investigate the most suitable fraction for dating, 112 measurements were obtained from three components within selected horizons: a fine fraction <0.2 mm, a coarse fraction >0.2 mm, and bulk material. We find site selection is critical, with locations surrounded by high-ground and/or relatively slowly accumulating sites more susceptible to the translocation of older carbon. Importantly, in locations with reduced potential for redeposition of material, our results show that there is no significant or systematic difference between ages derived from bulk material, fine or coarse (plant macrofossil) material, providing confidence in the resulting age model. Crucially, in areas comprising complex terrain with extreme relief, we recommend dating macrofossils or bulk carbon rather than a fine fraction, or employing comprehensive dating of multiple sedimentary fractions to determine the most reliable fraction(s) for developing a robust chronological framework.

Alkali- and Ca-rich smectites occur in association with Neogene lacustrine sedimentary rocks and high-K calc-alkaline volcanic rocks with compositions ranging from andesite to rhyolite in western Anatolia (Turkey). Major clay occurrences are associated predominantly with the Foça and Akçaköy ignimbrites and with the ignimbrites within the Rahmanlar pyroclastics. Experimental studies indicate that the main clay minerals present are Na- and Ca-smectite and subordinate illite, associated with silica polymorphs, trace clinoptilolite and chlorite. The authigenic minerals formed by weathering and metasomatic reactions between hot volcanic material and lake water. Smectite was produced as a result of argillic alteration of the volcanic glass and feldspars of the ignimbrites, Rahmanlar pyroclastics and reworked volcaniclastic sediments through chemical weathering and dissolution-precipitation processes and formed as authigenic phases both in terrestrial and nearby shallow lacustrine environments under prevalent humid or semi-humid climate during the Neogene.

Marine, freshwater and terrestrial ecosystems face increasing anthropogenic threats that are exacerbated by the ecological connectivity between realms; integrated land-sea management (ILSM) is a framework that can help address this connectivity. However, gaps in our knowledge regarding ILSM remain. This study reviewed 108 relevant studies to understand how ILSM is being utilized. Summarized are: (1) characteristics of integrated land-sea programs; (2) recommendations made from the literature for program planning, implementation and management; (3) how applied programs have been planned, implemented and managed; and (4) recommendations for undertaking ILSM. It was found that applied programs did not often adhere to the strategies recommended by theoretical papers. Applied programs were less likely than theoretical papers to specifically name the land-sea connection, over 50% did not apply a framework or governance approach, many did not include key stakeholders, and over 80% listed at least one conflict or hurdle that decreased program success. This study highlighted the difficulties of undertaking ILSM given the high number of stakeholders, government agencies and experts involved. Based on the findings, recommendations for future ILSM programs are provided.

We used stable isotope analysis (15N/14N) to characterize the trophic relationships of consumer communities of an aquatic food web (a permanent pond) and the adjacent terrestrial food web (secondary dry dipterocarp forest) from a seasonal tropical field site in north-eastern Thailand. In general, isotopic signatures of aquatic vertebrates were higher (δ15N range = 4.51–9.90‰) than those of invertebrates (δ15N range = 1.10–6.00‰). High 15N signatures identified water snakes and swamp eels as top predators in the pond food web. In the terrestrial food web 15N signatures of saprophagous litter invertebrates (diplopods, earthworms), termites, ants and beetle larvae were lower than in those of predatory invertebrates (scolopendrids, scorpions, whip spiders). Predatory terrestrial frogs and caecilians had lower 15N signatures than snakes, indicating that snakes are among the top predators in the terrestrial web. Based on the distribution of isotopic signatures, we estimated five trophic levels for both the aquatic and terrestrial food web. The food chains of a seasonal tropical site studied were rather short, which implies similarities to the structure of temperate food webs.

Substrate reaction forces (SRFs) were quantified for 502 forelimb and hindlimb contacts in two primate species, Eulemur fulvus and Lemur catta. Three individuals of each taxon were encouraged to traverse a force transducer. Reaction forces were evaluated for linear locomotion on runway and simulated arboreal substrates. Preferred gaits differed between substrates: galloping on the runway and walking on simulated arboreal substrates. Unlike vertical and fore–aft (FA) forces, mediolateral (ML) forces during linear locomotion were relatively independent of speed, which suggests balancing the centre of body mass in the coronal plane was not speed related. Since peak ML forces occasionally exceeded peak FA forces, ML forces were not of trivial importance during primate quadrupedal locomotion. Both lemurids regularly experienced lower ML peak forces during ‘arboreal’ than ‘terrestrial’ quadrupedalism, probably to minimize side-to-side fluctuations of their centre of mass over the simulated arboreal branch supports. Eulemur fulvus encountered greater ML peak forces in their forelimbs, while L. catta encountered greater hindlimb peak ML forces. Lemurids most frequently exerted medially directed peak side-to-side forces during arboreal quadrupedalism and laterally directed peak side-to-side forces during terrestrial quadrupedalism. The direction of hindlimb ML peak force, however, was less consistent than forelimb ML peak force regardless of substrate. The lemurs experienced oscillations in the direction of the forelimb and hindlimb ML force over the duration of support phase, suggesting that both pairs of limbs contributed to balance. More frequent changes in ML force direction of the hindlimb support the predominance of these limbs in keeping side-to-side balance. The results of our study suggest that ML forces warrant consideration in locomotion studies, especially when evaluating joint moments and bending regimes of long bones.

The Windyfield chert site is located 700 m NE of the original Rhynie chert locality at Rhynie, Aberdeenshire, Scotland. Originally identified by concentrations of surface float material, a drilling and trenching programme of the area in 1997 revealed a chert ‘pod’ in situ interbedded with fluvial/lacustrine sandstones and hydrothermally altered shales. Chert morphologies identified from float blocks and trench material range from tabular beds to lenticular pods displaying massive, nodular, laminated and brecciated fabrics, and geyserite splash textures. A suite of floral and faunal associations, when combined with distinctive macro- and microscopic chert textures, has been used to interpret depositional conditions. Palaeoenvironments ranged from terrestrial laminated, brecciated and vegetated sinter sheets to low-temperature pools and marginal aquatic settings. The flora comprises six higher land plant species, nematophytes, charophytes, various fungi and probable cyanobacteria. Arthropods include branchiopod crustaceans, a euthycarcinoid, trigonotarbid arachnids, centipedes, eoarthropleurids and a possible hexapod. The biota of the Windyfield chert is closely comparable to that found in the Rhynie chert. Together, the Windyfield and Rhynie cherts contain the most diverse associated fossil arthropod fauna of terrestrial and freshwater origin from rocks of comparable age anywhere in the world.