A diatom-inferred record of reduced effective precipitation during the Last Glacial Coldest Phase (28.8-18.0 cal kyr BP) and increasing Holocene seasonality at Lake Pupuke, Auckland, New Zealand

Journal of Paleolimnology

Volumn 48, Issue 4, 2012, Pages 801-817

  Stephens, Thomas ^a,b   Atkin, Daniel ^b   Cochran, Ursula ^c   Augustinus, Paul ^b   Reid, Michael ^d   Lorrey, Andrew ^e   Shane, Philip ^b   Street Perrott, Alayne ^f  

^a UNIVERSITY OF FLORIDA   (United States)

^b UNIVERSITY OF AUCKLAND   (New Zealand)

^c GNS SCIENCE   (New Zealand)

^d UNIVERSITY OF NEW ENGLAND   (Australia)

^e NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH   (New Zealand)

^f SWANSEA UNIVERSITY   (United Kingdom)

Author keywords

Climate and environmental change; Diatoms; New Zealand; Seasonality; Southern westerlies

Indexed keywords

CHLOROPHYLL A; CLIMATE CHANGE; DIATOM; HOLOCENE; LAST GLACIAL-INTERGLACIAL; NUTRIENT AVAILABILITY; PALEOPRODUCTIVITY; PHOSPHORUS; PRECIPITATION (CLIMATOLOGY); SEASONALITY; WESTERLY;

AUCKLAND; LAKE PUPUKE; NEW ZEALAND; NORTH ISLAND;

BACILLARIOPHYTA;

EID: 84869751941     PISSN: 09212728     EISSN: None     Source Type: Journal    
DOI: 10.1007/s10933-012-9645-y     Document Type: Article

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