The exposed nature of the northern Faroe Islands high relief landscape enabled widespread Holocene slope process activity and deposition of related landforms, which seem largely controlled by extreme meteorological conditions. Three different slope landforms – the large colluvial Glyvurs fan, the lower Marknastiggjur mountainside debris-flow deposits in the town of Klaksvik, and the mountain top aeolian sediment cover on Eidiskollur – were investigated by a combination of geomorphological, stratigraphic, sedimentological, chronological and modern process studies.

Sporadic Holocene snow-avalanche and debris-flow activity were documented, with sedimentation starting significantly before 8000 cal yr BP in the Glyvurs fan, which still sporadically experiences activity. The largest amounts of Holocene slope sedimentation seem to occur in colluvial fans, such as the Glyvurs fan, which are located below large dyke canyons, called gjogvs. The lower Marknastiggjur mountainside consists of mainly debris-flow deposits, which started before 7800 cal yr BP. A relatively small amount of precipitation, but with high precipitation intensity after a dry summer, triggered modern small-scale debris-flows in the northern islands, also at the Marknastiggjur mountainside, early in Autumn 2000. Extensive continuous mountaintop aeolian sedimentation from cliff weathering started around 6900 cal yr BP on the Eidiskollur peninsula.

No direct influence of settlement on slope process activity was found at the different investigated slope landforms in the northern Faroe Islands.

As an isolated island group lying off the NW European mainland which was uninhabited until the mid-first millennium AD, the Faroes offer a unique opportunity to study natural processes of Holocene ecosystem development in a region where anthropogenic activity is usually a complicating factor. In this paper new radiocarbon dates and pollen-analytical data from the island of Sandoy, in the centre of the Faroes archipelago, are presented. Together with existing pollen and plant macrofossil records, these data allow a reconstruction of patterns of Holocene vegetational and edaphic change. Basal peat dates indicate that large areas of blanket mire were established long before the first human settlement, demonstrating conclusively that human impact is not necessary for the development of such ecosystems. The timing of the initiation of the blanket peats varies markedly, both across the Faroes as a whole and at a landscape scale, with dates distributed evenly over 9000 years. This suggests that, in the Faroes at least, pedogenesis was more important than climatic change in determining the timing of the spread of blanket peat systems.

Archaeological investigations demonstrate that peoples first settled the Caribbean islands approximately 6000–7000 years ago. At least four major, and multiple minor, migrations took place over the next millennia by peoples from Mesoamerica and South America who practised various subsistence strategies and had different levels of technology. For decades, researchers have been interested in investigating how these groups adapted to and impacted insular environments through time. This paper combines archaeological, palaeoecological, historical, and modern biological data to examine the effects of humans on Caribbean island ecosystems using a historical ecology approach. By synthesising a wide range of data sources, we take a human/nature dialectical perspective to understanding how peoples adapted to and modified their environments. The data suggest that earlier foraging/fishing Archaic groups (ca. 6000–3000 BP), who used a stone tool and shell technology and transported few, if any non-indigenous plants or animals, still impacted island landscapes as evidenced by bird and sloth extinctions. As more advanced ceramic making horticulturalists entered the Antillean chain around 2500 BP, there is an observable change to island environments as a result of forest clearance, overexploitation of both terrestrial and marine resources, and growing populations. Palaeoecological and palaeoenvironmental records also suggest, however, that an increased moisture regime during the late Holocene probably led to a decrease in near-shore salinity and heavier sediment and nutrient loads in rivers. These conditions would have been exacerbated by land clearance for agriculture, leading to coastline progradation, increased turbidity, and mangrove development resulting in changes to the availability of resources for humans on some islands. Although prehistoric peoples in the Caribbean were certainly impacting their environments, it was not until Europeans arrived and population centres grew that intensive and widespread degradation of island landscapes and resources occurred. Modern ecological studies, along with historical and archaeological data, indicate that hundreds of species have been driven to extinction or extirpation – many others have significantly diminished in number, especially within the last two millennia.

The 1800 km-long Aleutian archipelago represents a model ecosystem to track human–environmental interactions across space and through time. Defining the southern margin of Beringia across which much of the early peopling of the Americas occurred, the Aleutians present a 9000 year record of human occupation in the eastern part of the island chain, and more than 3000 years in the west. Molecular evidence demonstrates: (1) that Aleuts shared common ancestry with Chukchi and Siberian Eskimos of Chukotka; (2) the original patterns of migration into the Aleutian islands were from the Alaskan peninsula in a westward direction with no evidence for island-hopping from Kamchatka; and (3) a highly significant statistical relationship between geography and genetics, based on mtDNA sequences, was observed despite previous population disruption. Historically, the Aleutian region is a rich ecotone, with ocean fisheries, abundant populations of large marine mammals, thick kelp forests, complex near-shore ecosystems and intertidal zones, spawning streams, and a highly diverse avian fauna. Each of these environments and resources has been pivotal in shaping the adaptive strategies of human occupants of the island chain since the initial colonisation of the Aleutians from the Alaskan Peninsula. In turn, Holocene human immigration, prehistoric cultural adaptations and subsequent historic events have had reciprocal impacts on the natural systems of the Aleutians.

We present the first record of Holocene and Pleistocene environmental change derived from the chemical and stable-isotope composition of a tropical cave guano sequence from Makangit Cave in northern Palawan (Philippines). The 180 cm sequence of guano, derived predominantly from insectivorous bats and birds, consists of two distinct units. An upper section of reddish-brown oxidised guano to 110 cm was deposited since the mid-Holocene while a lower section of black, reduced guano was deposited through the Last Glacial Maximum (LGM) to >30 000 BP. Carbon-isotope (δ13C) values in guano deposited during the LGM are as high as −13·5‰ indicating that a C4-dominated grassland existed in the area around the cave at this time. Guano δ13C values of − 25‰ to − 28‰ suggest that this open vegetation was replaced by C3-dominated closed tropical forest, similar to that of the present, by the mid-Holocene. The results suggest that the climate of northern Palawan was substantially drier at the LGM than is currently the case.

Campbell Island is a small, uninhabited peat-covered island lying in the cool southern ocean 600 km south of the New Zealand mainland. Dracophyllum scrub is the main cover from sea level to 200 m, above which tussock grassland, macrophyllous forbs and tundra dominate. Seven peat profiles from sea level to the tundra zone provide an elevational transect for pollen and charcoal records spanning the last 500 years. Scrub density was relatively low between 200 and 400 cal yrs BP, possibly due to Little Ice Age cooling, but had recovered by the time Europeans discovered the island in AD 1810. Burning and grazing during a brief farming episode (AD 1895–1931) severely reduced scrub and palatable grasses and forbs. Vegetation recovery is now well advanced following cessation of farming and the later elimination of all feral grazing animals, cats and rats. Climates were cool in the southwest Pacific during the farming period, and since AD 1970 the island has warmed by c. 0·5°C. However, there has been no upwards movement of the scrubline despite vigorous regeneration of scrub at lower altitudes. The island's cloudy, highly oceanic climate appears to offset increasing summer warmth, and scrubline is likely to rise only if clearer and less windy, as well as warmer, summers eventuate.

Oceanic islands offer outstanding ‘model systems' for investigating long-term dynamics between human populations and their ecosystems. Whilst the state factors involved in human-environment dynamics on islands are often simpler than on continents, the same essential processes are involved. This paper applies a comparative approach to understanding the reciprocal interactions between a set of four Polynesian island cases (Tikopia, Mangaia, Mangareva, Hawaiian Islands), over time scales of between one and three thousand years (kyr). In all cases, the island ecosystems were colonised by Polynesian populations derived from the same ancestral culture, with similar socioeconomic patterns. However, the ecosystems vary significantly in scale, geologic age, and other characteristics. Comparing the historical trajectories of these human–environment dynamics, as revealed by archaeological and palaeoecological study, provides insights into the relative impact of humans on pristine island ecosystems, the influence of environment on ecosystem vulnerability, and the ways in which societies have modified their economies, sociopolitical structures, and other aspects of culture in response to long-term environmental changes.

This paper draws on epistemology, theory, published data, hypothesis testing and synthesis to explore the predictive and explanatory power of a far-from-equilibrium interpretation of the history of human settlement on Rapa Nui. Our interpretation of the last 1500 years of human settlement on Rapa Nui provides an important competing hypothesis by which to test the explanatory power of earlier equilibrium interpretations of this history. Our evaluation of this competing hypothesis suggests that it provides, overall, a more satisfactory theory that has interesting implications for the goal of sustaining human civilisation.

Holocene sea-level changes affected people living in the Pacific Islands and their ancestors along the western Pacific Rim. Sea-level changes, particularly those that were rapid, may have led to profound and enduring societal/lifestyle changes. Examples are given of (1) how a rapid sea-level rise (CRE-3) about 7600 BP could ultimately have led to the earliest significant cross-ocean movements of people from the western Pacific Rim into the islands; (2) how mid to late Holocene sea-level changes gradually created coastal environments on Pacific Islands that were highly attractive to human settlers; (3) a hypothesis that rapid sea-level fall during the ‘AD 1300 Event' brought about widespread disruption to trajectories of cultural evolution throughout the Pacific Islands; and (4) the effects of recent and likely future sea-level rise on Pacific Island peoples.