For example, the warm - water phase of ENSO is associated with large - scale changes in
plankton abundance and associated impacts on food webs (Hays et al., 2005), and changes to behaviour (Lusseau et al., 2004), sex ratio (Vergani et al., 2004) and feeding and diet (Piatkowski et al., 2002) of marine mammals.
The most important changes in
plankton abundance arise from upwelling.
Or does the community just ignore the Bass River record entirely because
plankton abundance and / or sedimentation could have been temporarily and drastically disrupted at this site in response to the environmental effects of the PETM?
With warmer equatorial waters reducing
plankton abundance and spurring many fish species, notably bigeye and skipjack tuna, to migrate toward the poles, the waters around Wake and Johnston, 1600 kilometers north of the equator, «are precisely where you want to have a protected area,» says Robert Richmond of the University of Hawaii at Mānoa.
They reported this finding in July after analyzing 50 - plus years of data on light penetration of the ocean surface and
plankton abundance in water samples.
Not exact matches
Satellite images as well as maps of chlorophyll
abundance appear to show that the iron did indeed fuel a
plankton bloom in August.
A wet suit (provided to you) may be required while snorkeling during those months, but the upside of colder water is that the cold current brings in huge quantities of
plankton, which attract hungry marine life in
abundance.
Elsewhere in the oceans, the environmental changes during the PETM led to shifts in the distribution of
plankton groups, with tropical species invading the high latitudes and high - latitude species dwindling in
abundance.
They need abundant amounts of fish and
plankton and krill and so on so it is necessary for them to not only find this
abundance but to «farm» it.
The change was measured using the orbiting SeaWiFS instrument, which can measure the
abundance of
plankton by tracking color differences in sea water.
Other aspects of global warming's broad footprint on the world's ecosystems include changes in the
abundance of more than 80 percent of the thousands of species included in population studies; major poleward shifts in living ranges as warm regions become hot, and cold regions become warmer; major increases (in the south) and decreases (in the north) of the
abundance of
plankton, which forms the critical base of the ocean's food chain; the transformation of previously innocuous insect species like the Aspen leaf miner into pests that have damaged millions of acres of forest; and an increase in the range and
abundance of human pathogens like the cholera - causing bacteria Vibrio, the mosquito - borne dengue virus, and the ticks that carry Lyme disease - causing bacteria.
If our climate continues to warm at today's rate, scientists expect North Sea
plankton that respond to temperature cues to bloom even earlier in the coming decades.7 With a growing mismatch in life cycles among various species of
plankton, as well as further climate - induced shifts in their
abundance and distribution, effects on the North Sea ecosystem — including cod — are projected to be considerable.7, 8
Marine mammals, birds, cetaceans and pinnipeds (seals, sea lions and walruses), which feed mainly on
plankton, fish and squid, are vulnerable to climate change - driven changes in prey distribution,
abundance and community composition in response to climatic factors (Learmonth et al., 2006).