1994
DOI: 10.1016/0277-3791(94)90030-2
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Direct correlation of terrestrial and marine paleoclimatic records from four glacial-interglacial cycles — DSDP site 594 Southwest Pacific

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Cited by 98 publications
(64 citation statements)
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“…Similar Last Glaciation occurrences of Empodisma are recorded both on the Bay of Plenty coast ) and offshore cores DSDP 594 and S803 (Heusser & van der Geer 1994;Wright et al 1995). However, Empodisma pollen is sometimes found in quantity in estuarine sediments in catchments with no extant source of this pollen type (McGlone unpubl.…”
Section: Pollen and Spore Representationmentioning
confidence: 54%
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“…Similar Last Glaciation occurrences of Empodisma are recorded both on the Bay of Plenty coast ) and offshore cores DSDP 594 and S803 (Heusser & van der Geer 1994;Wright et al 1995). However, Empodisma pollen is sometimes found in quantity in estuarine sediments in catchments with no extant source of this pollen type (McGlone unpubl.…”
Section: Pollen and Spore Representationmentioning
confidence: 54%
“…Analysis of carbon isotopes, sediment, and faunal variations gives valuable additional information as to water mass status, sea-surface temperatures, and influx of terrestrially derived sediments (Stewart & Neall 1984;Nelson et al 1985;Dudley & Nelson 1988;Weaver et al 1998). Several marine cores close to the New Zealand mainland have been pollen analysed: a 60 000 yr record has been produced from two cores off northeast New Zealand (Wright et al 1995); a 350 000 yr record spanning four glacial-interglacial cycles off southeast New Zealand (Heusser & van der Geer 1994); and a short, late Holocene core from coastal waters near Poverty Bay (Wilmshurst et al 1999).…”
Section: Introductionmentioning
confidence: 99%
“…The Wainoni Gravel at depths of 140-150 m below Christchurch is assigned to the Nemona Glaciation. Suggate (1990) and Pillans (1991) noted that the terrestrial record of glacial and interglacial events from the early-mid Pleistocene is largely filled in North Island by uplifted Wanganui Basin marine sediments and in South Island by marine sediments of Site 594 of the Deep Sea Drilling Project Leg 90, located c. 300 km east of South Island in a water depth of 1204 m (Nelson et al 1985;Black et al 1988;Heusser & van de Geer 1994). In this core, indirect evidence of glaciations and interglacials is provided Fig.…”
Section: Introductionmentioning
confidence: 99%
“…Il devient donc partie intégrante de la neige marine et traverse la colonne d'eau avec une vitesse de sédimentation relativement importante (estimée à ~100 m/jour dans la colonne d'eau atlantique) avant de se déposer au fond des océans (Hooghiemstra et al, 1992). Des études portant sur la pluie pollinique récente en domaine marin que ce soit sur la marge ibérique (Turon, 1984a ;Naughton et al, 2007) mais aussi dans le Golfe de Gascogne (Turon, 1984b), en Méditerranée (Koreneva, 1971), sur la marge africaine (Hooghiemstra et al, 1986 ;Dupont & Wyputta, 2003), ou sur les marges ouest et est de l'Amérique du Nord et dans le golfe du Mexique (Heusser & Balsam, 1977 ;Heusser, 1985 ;Heusser & Van de Geer, 1994) montrent que le pollen des sédiments océaniques reflète une image intégrée de la végétation régionale du proche continent et, par conséquent, les paramètres climatiques sous lesquels cette végétation s'est développée. En particulier, Naughton et al (2007) démontrent par la comparaison de spectres polliniques actuels de l'océan profond, d'estuaires et d'échantillons de surface continentaux que le signal pollinique de la marge ibérique représente de façon fiable la végétation du proche continent.…”
Section: -Les Archives Polliniques Marinesunclassified