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Why is pollen yellow? And why are there so many species in the tropical rain forest

Journal of biogeography, 2011-05, Vol.38 (5), p.809-816

Flenley, John R

2011

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The last glacial maximum climatic conditions on Easter Island

Quaternary international, 2008-06, Vol.184 (1), p.166-176

2008

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The Equatorial Rain Forest: A Geological History

Flenley, John R

1, 1979

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Evidence for continued disturbance of upland rain forest in Sumatra for the last 7000 years of an 11,000 year record

Palaeogeography, palaeoclimatology, palaeoecology, 2001-07, Vol.171 (3), p.289-305

2001

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Towards automation of palynology 3: pollen pattern recognition using Gabor transforms and digital moments

Journal of quaternary science, 2004-12, Vol.19 (8), p.763-768

2004

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Recent expansions of glacial lakes in the Bhutan Himalayas

Quaternary international, 2008-06, Vol.184 (1), p.177-186

Komori, Jiro

2008

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Untangling the causes of vegetation change in a 5,300 year pollen record at Tiniroto Lakes, Gisborne, New Zealand

Vegetation history and archaeobotany, 2014-03, Vol.23 (2), p.87-96

2014

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Towards automation of palynology 2: the use of texture measures and neural network analysis for automated identification of optical images of pollen grains

Journal of quaternary science, 2004-12, Vol.19 (8), p.755-762

2004

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Tropical forests under the climates of the last 30,000 years

Climatic change, 1998-07, Vol.39 (2-3), p.177-197

Flenley, J.R. (Massey Univ., Palmerston North (New Zealand). Dept. of Geography)

1998

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Towards automation of palynology 1: analysis of pollen shape and ornamentation using simple geometric measures, derived from scanning electron microscope images

Journal of quaternary science, 2004-12, Vol.19 (8), p.745-754

2004

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The Late Quaternary vegetational and climatic history of Easter Island

Journal of quaternary science, 1991-06, Vol.6 (2), p.85-115

1991

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Last glacial maximum (LGM) vegetation changes in the Atlantic Forest, southeastern Brazil

Quaternary international, 2008-06, Vol.184 (1), p.195-201

2008

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GUEST EDITORIAL: Why is pollen yellow? And why are there so many species in the tropical rain forest?

Journal of biogeography, 2011-05, Vol.38 (5), p.809-816

Flenley, John R.

2011

Volltextzugriff (PDF)

Why is pollen yellow? And why are there so many species in the tropical rain forest?: Why is pollen yellow?

Journal of biogeography, 2011-05, Vol.38 (5), p.809-816

Flenley, John R.

2011

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Spatial biome changes in southwestern Japan since the Last Glacial Maximum

Quaternary international, 2008-06, Vol.184 (1), p.84-93

2008

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Anomalous Radiocarbon Dates from Easter Island

Radiocarbon, 2004, Vol.46 (1), p.395-405

2004

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Recovery of DNA and pollen from New Zealand lake sediments

Quaternary international, 2008-06, Vol.184 (1), p.139-149

2008

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Late Quaternary landscape and vegetation diversity in a North European perspective

Quaternary international, 2008-06, Vol.184 (1), p.187-194

2008

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Late Holocene vegetation changes and human impact in the Changbai Mountains area, Northeast China

Quaternary international, 2008-06, Vol.184 (1), p.94-108

2008

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Social change in late Holocene mainland SE Asia: A response to gradual climate change or a critical climatic event?

Quaternary international, 2008-06, Vol.184 (1), p.11-23

Boyd, W.E.

2008

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Vegetation changes and their climatic implication for the late Pleistocene at Lake Poukawa, Hawkes Bay, New Zealand

Global and planetary change, 2002-07, Vol.33 (3), p.269-282

2002

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Late Quaternary vegetational history of the Central Highlands of Sumatra. II. Palaeopalynology and vegetational history

Journal of biogeography, 1988-07, Vol.15 (4), p.555-578

1988

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Holocene vegetational and climatic history, Sponge Swamp, Haast, south-western New Zealand

Quaternary international, 2008-06, Vol.184 (1), p.129-138

2008

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Late Glacial beech forest: an 18,000–5000-BP pollen record from Auckland, New Zealand

Global and planetary change, 2002-07, Vol.33 (3), p.315-327

2002

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A modified sampler for uncontaminated DNA cores from soft sediments

Journal of archaeological science, 2006-04, Vol.33 (4), p.573-574

2006

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Why is pollen yellow? And why are there so many species in the tropical rain forest

The last glacial maximum climatic conditions on Easter Island

The Equatorial Rain Forest: A Geological History

Evidence for continued disturbance of upland rain forest in Sumatra for the last 7000 years of an 11,000 year record

Towards automation of palynology 3: pollen pattern recognition using Gabor transforms and digital moments

Recent expansions of glacial lakes in the Bhutan Himalayas

Untangling the causes of vegetation change in a 5,300 year pollen record at Tiniroto Lakes, Gisborne, New Zealand

Towards automation of palynology 2: the use of texture measures and neural network analysis for automated identification of optical images of pollen grains

Tropical forests under the climates of the last 30,000 years

Towards automation of palynology 1: analysis of pollen shape and ornamentation using simple geometric measures, derived from scanning electron microscope images

The Late Quaternary vegetational and climatic history of Easter Island

Last glacial maximum (LGM) vegetation changes in the Atlantic Forest, southeastern Brazil

GUEST EDITORIAL: Why is pollen yellow? And why are there so many species in the tropical rain forest?

Why is pollen yellow? And why are there so many species in the tropical rain forest?: Why is pollen yellow?

Spatial biome changes in southwestern Japan since the Last Glacial Maximum

Anomalous Radiocarbon Dates from Easter Island

Recovery of DNA and pollen from New Zealand lake sediments

Late Quaternary landscape and vegetation diversity in a North European perspective

Late Holocene vegetation changes and human impact in the Changbai Mountains area, Northeast China

Social change in late Holocene mainland SE Asia: A response to gradual climate change or a critical climatic event?

Vegetation changes and their climatic implication for the late Pleistocene at Lake Poukawa, Hawkes Bay, New Zealand

Late Quaternary vegetational history of the Central Highlands of Sumatra. II. Palaeopalynology and vegetational history

Holocene vegetational and climatic history, Sponge Swamp, Haast, south-western New Zealand

Late Glacial beech forest: an 18,000–5000-BP pollen record from Auckland, New Zealand

A modified sampler for uncontaminated DNA cores from soft sediments

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