-
Accumulation rate, carbon geochemistry and clay mineralogy of ODP Site 181-11...
Site 1123 is located on the northeastern flank of the Chatham Rise. Sedimentological and clay mineralogical analyses indicate a very fine grained carbonate-rich sediment.... -
Natural gamma ray and stable isotope record of ODP Site 181-1119
Ocean Drilling Program Site 1119 is ideally located to intercept discharges of sediment from the mid-latitude glaciers of the New Zealand Southern Alps. The natural gamma ray... -
Late Quaternary radiolarian assemblages of ODP Site 181-1124
Abundant and diverse polycystine radiolarian faunas from ODP Leg 181, Site 1123 (0-1.2 Ma at ~21 kyr resolution) and Site 1124 (0-0.6 Ma, ~5 kyr resolution, with a disconformity... -
Locations of geochemical samples and tephra from ODP Site 181-1123
Approximately one thousand sediment samples from ODP Site 1123 on the Chatham Rise, east of New Zealand, have been examined for inorganic elemental concentrations. ODP 1123... -
Pleistocene rhyolithic tephra of ODP Leg 181 sites
Taupo Volcanic Zone (TVZ), in the North Island, New Zealand, is arguably the most active Quaternary rhyolitic system in the world. Numerous and widespread rhyolitic tephra... -
Sea-surface temperature reconstruction in the Southwest Pacific
Uniquely in the Southern Hemisphere the New Zealand micro-continent spans the interface between a subtropical gyre and the Subantarctic Circumpolar Current. Its 20° latitudinal... -
Pliocene foraminifera and SST changes in ODP Site 184-1125
Planktonic foraminiferal census counts were converted to sea surface temperature (SST) estimates using the modern analogue technique (MAT) for the middle-late Pliocene (4.0-2.37... -
Age data of ODP Site 181-1124
ODP Site 1124, located 600 km east of the North Island of New Zealand, records post-middle Oligocene variations in the Pacific Deep Western Boundary Current (DWBC) and New... -
10Be/9Be-based chronostratigraphy of ODP Hole 181-1121B from the Southwest Pa...
A 10Be/9Be-based chronostratigraphy has been determined for ODP 181, Site 1121 sediment core, recovered from the foot of the Campbell Plateau, Southwest Pacific Ocean. This core... -
Distribution of planktonic foraminifera during the Mid-Pleistocene of ODP Sit...
Planktonic foraminiferal assemblages and artificial neural network estimates of sea-surface temperature (SST) at ODP Site 1123 (41°47.2'S, 171°29.9'W; 3290 m deep), east of New... -
Glacial-interglacial record of ODP Site 181-1119 in the Canterbury Bright, So...
Ocean Drilling Program (ODP) Site 1119 is located at water depth 395 m near the subtropical front (STF; here represented by the Southland Front), just downslope from the shelf... -
Mid-Pleistocene benthic foraminiferal record in the Southwest Pacific
Benthic foraminiferal faunas from three bathyal sequences provide a proxy record of oceanographic changes through the mid-Pleistocene transition (MPT) on either side of the... -
Late Quaternary benthic foraminiferal record of the Bounty Trough, east of Ne...
The Bounty Trough, east of New Zealand, lies along the southeastern edge of the present-day Subtropical Front (STF), and is a major conduit via the Bounty Channel, for... -
Quaternary radiolarian counts from Site 181-1123
In the present work Quaternary radiolarian assemblages from the Southwest Pacific were investigated due to their importance for correlation and identification of climatic... -
Planktic foraminiferal and sea surface temperature record during the last 1 M...
Planktic foraminiferal faunas and modern analogue technique estimates of sea surface temperature (SST) for the last 1 million years (Myr) are compared between core sites to the... -
Distribution of benthic foraminifera in surface sediments east of New Zealand...
This study investigates which combination of environmental factors most strongly influences the distribution patterns of benthic foraminferal tests (>0.63 µm) in a region... -
Paleocene radiolarian distribution and biostratigraphy from offshore eastern ...
A 100-m-thick Paleocene sequence of mainly pelagic sediments at ODP Site 1121, on the eastern flanks of the Campbell Plateau, contains few to common radiolarians of relatively... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Correlations between the proxy SST anomalies (annual, boreal summer and borea...
This dataset has no description
-
Last interglacial and penultimate glacial sea surface temperature anomalies f...
Southern Ocean marine sediments provide an important archive of Quaternary glacial-interglacial climate changes. Sea surface temperature (SST) reconstructions in the Southern...