(Table 14B) Occurrences of planktonic foraminifers in DSDP Hole 592, samples 592-30-CC through 592-41-CC
收藏PANGAEA2024-09-14 收录
官方服务:
资源简介:
X = present, - = absent, cf. = confer.
应用场景:
相关数据集
NOAA/WDS Paleoclimatology - Global Hydro-sensitive Coral d18O Records for Improved High-Resolution Temperature and Salinity Reconstructions
Stable oxygen isotopic ratios in corals (d18Ocoral) are commonly utilized to reconstruct climate variability beyond the limit of instrumental observations. These measurements provide constraints on pa
DataCite Commons2025-10-15 更新40
Radiolaria abundance of Hole 54-421
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
PANGAEA10
Magnesium/Calcium ratios and sea surface temperature estimation for sediments...
We use a multiproxy approach to monitor changes in the vertical profile of the Indonesian Throughflow as well as monsoonal wind and precipitation patterns in the Timor Sea on...
B2FIND10
Relative abundance of coccosphere-units at site GIK23414
Age given in calendar years. Coccosphere-unit: Conversion of coccoliths to hypothetical coccospheres by taking an average number of coccoliths per coccosphere.
PANGAEA2002-01-01 更新20
(Table T3) Ages of the Miocene planktonic foraminifer zonal boundaries from ODP Sites 184-1146 and 184-1148
DEPTH, sediment is given in mcd. At Site 184-1148, the Zone N12/N13 boundary is undecided, and the Zone N6/N7 boundary at 367 mcd is estimated to be ~18000 ka on the local FO of Globigerinatella insue
PANGAEA2004-01-01 更新10



