Dataset - B2FIND

Palynology (relative abundance) of IODP Hole 381-M0079A

Only species with relative abundances >2.5 are shown.D = dominant, A = abundant, C = common, F = few, R = rare.

Palynology (relative abundance) of IODP Hole 381-M0078B

Only species with relative abundances >2.5 are shown.D = dominant, A = abundant, C = common, F = few, R = rare.

Palynology (relative abundance) of IODP Hole 381-M0078A

Only species with relative abundances >2.5 are shown.D = dominant, A = abundant, C = common, F = few, R = rare.

Palynology grains (concentrations) of IODP Hole 381-M0079A

Only species with relative abundances >2.5 are shown.

Palynology grains (concentrations) of IODP Hole 381-M0078B

Only species with relative abundances >2.5 are shown.

Palynology grains (concentrations) of IODP Hole 381-M0078A

Only species with relative abundances >2.5 are shown.

Palynology of marine sediment core SBQW4, Saldanha Bay (South Africa), early ...

A multi-proxy study of an offshore core in Saldanha Bay (South Africa) provides new insights into fluvial deposition, ecosystems, phytogeography and sea-level history during the...

Effects of acute ocean acidification on spatially-diverse polar pelagic foodw...

The polar oceans are experiencing some of the largest levels of ocean acidification (OA) resulting from the uptake of anthropogenic carbon dioxide (CO2). Our understanding of...

Phytoplankton responses and associated carbon cycling during shipboard carbon...

The ongoing oceanic uptake of anthropogenic carbon dioxide (CO2) is significantly altering the carbonate chemistry of seawater, a phenomenon referred to as ocean acidification....

Fossil occurrence of pollen from IODP Hole 337-C0020A

Geocode = [m, CMP] Top Depth DSF, MSF, WSF and CSF-B.999.999 = reworked.

Dinoflagellate cyst accumulation rates of ODP Hole 146-893A from Santa Barbar...

The dinoflagellate cyst record from Ocean Drilling Program Hole 893A, Santa Barbara Basin, southern California, is examined at millennial-scale resolution for the past 40 kyr....

Occurence of marine palynomorphs of sediment core CRP-1 (Table 1)

The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section rather than the anticipated Palaeogene sediments. Initial palynologic study...