Top Banner
It’s a small world… or: Just because you can’t see it doesn’t mean it’s not there!
31
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

It’s a small world…

or:

Just because you can’t see it doesn’t mean it’s not there!

Page 2: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

What are Protozoa ?• Protozoa are single-celled organisms• One cell can perform all the living functions

(feeding, movement, reproduction) multicellular organisms – such as worms or humans - need a large number of cells for

• Protozoa have developed many different ‘ways of life’ (parasitic, free-living) in terrestrial and marine environments

• They are everywhere!

Page 3: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

What are Foraminifera ?

• Foraminifera are a group of Protozoa that are exclusively marine

• There are pelagic and benthic Foraminifera• They occur everywhere in the oceans• Forams are particularly abundant in low

temperature environments – e.g. the deep sea and polar seas – they appear to be the most common group of protozoa in Antarctic benthic environments!

Page 4: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 5: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

There are different kinds of Forams…

…some Forams are soft-bodied – they have an organic wall…

Page 6: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 7: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 8: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

…agglutinated Foraminifera make their tests out of sediment particles…

Page 9: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 10: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 11: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

…calcareous Foraminifera have shells made from calcium carbonate…

Page 12: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 13: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 14: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 15: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

Investigates the impact of food input on the benthic environment and the organisms living on the

Western Antarctic Peninsula shelf.

FOODBANCS:Food for the Benthos on theAntarctic Continental ShelfPIs Craig Smith, UH and Dave DeMaster, NCSU

1999-2000

Page 16: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 17: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

• Foraminifera show a strong specific response to pulsed food input

• They are able to ingest a large part of freshly deposited organic matter quickly

• Forams respond directly to food availability - other groups, e.g. nematode or polychaete worms, show a delayed response or no response at all.

Why Forams?

Page 18: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

What’s special about Forams?

• Being Protozoa, they can reproduce much faster than metazoa (asexual multiple fission)

• A solid calcareous or agglutinated test provides protection against environmental factors and (arguably) predators

• Forams have a high potential turnover rate - they can ‘burn’ a high amount of organic matter in a short period of time

• Their reticulopodial net is a highly efficient food gathering apparatus (conveyor-belt movement)

Page 19: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 20: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

FOODBANCS:Abundances of Foraminifera in the

>300µm size class

• Agglutinated foraminifera are more abundant than metazoa in the macrobenthic size class (>300 µm) in the topmost sediment layer (0-0.5 cm)

• Metazoan organisms are more abundant in the 0.5-1.0 cm layer below

• Organic matter from the spring phytoplankton bloom is most likely be processed to a great extent by foraminifera before metazoan organisms can get to it

Page 21: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

It’s not just about quantity!

Page 22: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

Food that’s good for you(and other critters):

Polyunsaturated Fatty Acids (PUFAs)

• PUFAs are a group of fatty acids – components of fats and oils – which are only produced by a small number of organisms, but needed by many

• In the marine environment, photosynthetic organisms such as diatoms and flagellates produce PUFAs in high amounts

Page 23: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

What are PUFAs good for?

• PUFAs are important for certain cell membrane properties, e.g. preservation of membrane fluidity under high pressure or low temperature (deep-sea, Antarctic!!)

• Certain fish species need PUFAs in neural tissue (retinas and brain)

• PUFAs are precursors for a number of animal hormones

• Phytoplankton with high PUFA content supports higher zooplankton biomass – the availability of PUFAs is a limiting factor

Page 24: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

What happens to these fatty acids?

Page 25: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 26: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare
Page 27: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

FOODBANCS:results from lipid analysis

• Three of the most abundant species of Foraminifera feed very selectively on certain components of freshly deposited organic matter

• There is some indication that certain species ingest and decompose that part of the phytodetritus which is rich in PUFAs and thus make it unavailable for other organisms

Page 28: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

And now…

Page 29: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

Objectives at Palmer

• Time series: development of fatty acid profiles of an abundant calcareous foraminiferal species – Globocassidulina crassa - in January-February

• Feeding experiments on G. crassa – decomposition of the ‘high quality’ part of phytoplankton?

Suhr & Pond (2006) Deep Sea Research Part II, Volume 53, Issues 8-10

Page 30: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

So…

Foraminifera have a potentially very important and complex role in areas with a pulsed food input such as the

Antarctic.

Page 31: Antarctic benthic foraminifera   austral summer 2001-2002 slideshare

Figure 4: MDS plot of replicate samples; = phytodetritus, = Gobocassidulina subglobosa, = Quinqueloculina sp., = Thurammina sp. (Stress = 0.09)

Suhr et al. (2003) MEPS Vol. 262: 153–162