5,978 Works

Appendices to The Settlement History of the Vrokastro Area and Related Studies

Barbara J. Hayden

Tables from Chapter 9

Barbara J. Hayden

Tables from Chapter 13

Barbara J. Hayden

Tables from Chapter 14

Barbara J. Hayden

Tables from Chapter 3

Barbara J. Hayden

Tables from Chapter 11

Barbara J. Hayden

Tables from Chapter 12

Barbara J. Hayden

Tables from Chapter 5

Barbara J. Hayden

Tables from Chapter 7

Barbara J. Hayden

Tables from Chapter 6

Barbara J. Hayden

Tables from Chapter 2

Barbara J. Hayden

Tables from Chapter 4

Barbara J. Hayden

Vrokastro Archaeological Survey Project Website

Hayden, Barbara J., AUTHOR; Dierckx, Heidi, AUTHOR; Harrison, George W. M., AUTHOR; Moody, Jennifer, AUTHOR; Postma, George, AUTHOR; Rackham, Oliver, AUTHOR; Stallsmith, Allaire B., AUTHOR

Tables from Chapter 8

Barbara J. Hayden

Chart 10.1 Relevant Epigraphical Data for the Region Istron

Stallsmith, Allaire B., AUTHOR; Hayden, Barbara J., AUTHOR

POLLEN, MACROFLORAL, PHYTOLlTH, AND PROTEIN RESIDUE ANALYSIS AT SITE 42GR3222, MOAB, UTAH

Puseman, Kathryn, AUTHOR (PaleoResearch Institute); Cummings, Linda Scott, AUTHOR (PaleoResearch Institute)

POLLEN AND MACROFLORAL ANALYSIS AT THE VIRGIN VILLAGE SITE, 42WS4335, SOUTHWEST UTAH

Puseman, Kathryn, AUTHOR (PaleoResearch Institute); Cummings, Linda Scott, AUTHOR (Null)

(Table 1) Different age analysis from sediment cores XP98-PC-4 and XP98-PC-2

Osamu Seki, Kimitaka Kawamura, Minoru Ikehara, Takeshi Nakatsuka & Tadamichi Oba
Sea-surface temperatures (SSTs) in the Sea of Okhotsk were reconstructed based on alkenone unsaturation indices in two sediment cores. Alkenone-SSTs were found to range from 3 to 9 °C over the last 85 kyr with higher SST values in warm periods: Holocene and the oxygen isotope stage (OIS) 5a. In the last glacial periods (OIS 4 and 3), average alkenone SST was estimated to be 4 °C, which was 4 °C lower than the Holocene...

Sea surface temperature and age analysis from sediment core KT94-15_PC-9, XP98-PC-4 and XP98-PC-2

Osamu Seki, Kimitaka Kawamura, Minoru Ikehara, Takeshi Nakatsuka & Tadamichi Oba
The Japan Sea experienced bottom water anoxia at the last glacial maximum (LGM) since it is surrounded by four shallow straits, the sill depths of which are close to, or shallower than, the drop in sea level (~120 m) that occurred then. A distinctive negative d18O excursion of planktonic foraminifera also took place during the LGM. This excursion has been interpreted from foraminiferal data as recording a drop in the paleosalinity of surface waters on...

Age and sea surface temperature from sediment core KT94-15_PC-9

Osamu Seki, Kimitaka Kawamura, Minoru Ikehara, Takeshi Nakatsuka & Tadamichi Oba

Age and sea surface temperature from sediment core XP98-PC-4

Osamu Seki, Kimitaka Kawamura, Minoru Ikehara, Takeshi Nakatsuka & Tadamichi Oba

Age and sea surface temperature from sediment core XP98-PC-2

Osamu Seki, Kimitaka Kawamura, Minoru Ikehara, Takeshi Nakatsuka & Tadamichi Oba

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