Palynomorph evidence for tropical climate stability in the Gulf of Papua, Papua New Guinea, over the latest marine transgression and highstand (14,500 years BP to today)

Holocene · Marine transgression · Palynology · Pollen · Radiocarbon dating · Sea level · Sediment · Stable isotope ratio · Younger Dryas · δ18O · Geological and Geophysical Studies · Geological formations and processes · Geology and Paleoclimatology Research · Ecology · Geology · Oceanography · Paleontology

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• Deciphering the Holocene environmental changes and anthropogenic impacts on the Kornati Archipelago (central Mediterranean) through multi-proxy sediment core analysis

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• Origins of Agriculture at Kuk Swamp in the Highlands of New Guinea

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• Rapid Flooding of the Sunda Shelf

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• Late Holocene flooding history of a tropical river in western India in response to southwest monsoon fluctuations

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• Pollen quantitative distribution in marine and fluvial surface sediments from the northern South China Sea

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• The palaeoenvironments of Kuk Swamp from the beginnings of agriculture in the highlands of Papua New Guinea

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• Holocene pollen records from Caution Bay, southern mainland Papua New Guinea

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• Agricultural emergence and transformation in the Upper Wahgi valley, Papua New Guinea, during the Holocene

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• A late-Holocene palaeoecological record from Ambra Crater in the highlands of Papua New Guinea and implications for agricultural history

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• Vegetation change following mid-Holocene marine transgression of the Torres Strait shelf

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