The planktonic foraminiferan (protozoan) Globigerina bulloides.  It tolerates the global range of sea surface temperatures, salinity, temperature, and density stratification and is not limited by these physical properties. Globigerina bulloides is most abundant in water masses at high southern latitudes and has distinct maxima in high northern latitudes and low latitude upwelling regions. Its geographic distribution and data from other authors suggest a preference for productive environments (Brock et al., 1992; Duplessy et al., 1981; Hemleben et al., 1989; Kipp, 1976; Thiede, 1983; van Leeuwen, 1989; Zhang, 1985) where G. bulloides may be related to the phytoplankton bloom succession
Globigerina_Sea_World_2004_07_20--053
Globigerina_Sea_World_2004_07_20--051
Globigerina Sea_World_2004_07_20--238
Globigerina FOUR 2006 02-09 Zuma--018mod
Globigerina FOUR 2006 02-09 Zuma--017mod
Globigerina Microplankton 2006 02-09 Zuma-030
Globigerina division Sea_World_2004_07_20--247
Globigerina FOUR 2006 02-09 Zuma--017
The planktonic foraminiferan (protozoan) Globigerina bulloides. It tolerates the global range of sea surface temperatures, salinity, temperature, and density stratification and is not limited by these physical properties. Globigerina bulloides is most abundant in water masses at high southern latitudes and has distinct maxima in high northern latitudes and low latitude upwelling regions. Its geographic distribution and data from other authors suggest a preference for productive environments (Brock et al., 1992; Duplessy et al., 1981; Hemleben et al., 1989; Kipp, 1976; Thiede, 1983; van Leeuwen, 1989; Zhang, 1985) where G. bulloides may be related to the phytoplankton bloom succession
The planktonic foraminiferan (protozoan) Globigerina bulloides.  It tolerates the global range of sea surface temperatures, salinity, temperature, and density stratification and is not limited by these physical properties. Globigerina bulloides is most abundant in water masses at high southern latitudes and has distinct maxima in high northern latitudes and low latitude upwelling regions. Its geographic distribution and data from other authors suggest a preference for productive environments (Brock et al., 1992; Duplessy et al., 1981; Hemleben et al., 1989; Kipp, 1976; Thiede, 1983; van Leeuwen, 1989; Zhang, 1985) where G. bulloides may be related to the phytoplankton bloom succession
The planktonic foraminiferan (protozoan) Globigerina bulloides. It tolerates the global range of sea surface temperatures, salinity, temperature, and density stratification and is not limited by these physical properties. Globigerina bulloides is most abundant in water masses at high southern latitudes and has distinct maxima in high northern latitudes and low latitude upwelling regions. Its geographic distribution and data from other authors suggest a preference for productive environments (Brock et al., 1992; Duplessy et al., 1981; Hemleben et al., 1989; Kipp, 1976; Thiede, 1983; van Leeuwen, 1989; Zhang, 1985) where G. bulloides may be related to the phytoplankton bloom succession
See photo in original gallery.