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Extra resources for Ocean Hydrodynamics: Ecohydrodynamics 12th: International Colloquium Proceedings

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The e f f e c t i v e r a t e of v e r t i c a l mixing on Georges Bank h a s been e s t i m a t e d ( F a l k o w s k i , p e r s o n a l cm sec-’ i n c o n t r a s t t o a s e a s o n a l u p w e l l i n g v e l o c i t y communication) t o be of $10-2 cm sec-1 o f f Oregon. Although t h e s o u r c e w a t e r s f o r Georges Bank c o n t a i n less n i t r a t e ( F i g . 1 6 ) than c o a s t a l u p w e l l i n g water o f f Oregon ( F i g . 200-250 g C m-2 y r - l on t h e Oregon and N e w York s h e l v e s (Walsh, 1 9 8 0 b ) .

8 of s e d i - o f s e d i m e n t s of t h e o u t e r con- (50-100 m ) between t h e M i s s i s s i p p i D e l t a and t h e Rio Grande (Hedges and P a r k e r , 1976). The Holocene s e d i m e n t s (%0-60 cm) of t h e upper s l o p e ( P a r k e r e t a l . 0), P l e i s t o c e n e s e d i m e n t s (%60 t o 1000 c m ) have 6 13C ( - 2 2 . 0) ( % 1 0 - 1 2 ) v a l u e s t h a t may be of t e r r e s t r i a l o r i g i n (Newman e t a l . , than j u s t r e f l e c t i o n s of d i a g e n e s i s (Degens, 1 9 7 0 ) .

T h a n 1 ug-at NO3 k-l found a t t h e i r b o u n d a r i e s ( F i g . 9 ) . 1 9 8 0 ) , w i t h less Diatom blooms of 5 Vq Chl Q-l h a v e been found a s s o c i a t e d w i t h t h e n i t r a t e i n p u t from eddy-induced upw e l l i n g a t t h e s h e l f break o f f Florida-Georgia (Atkinson e t a l . , 1980). Without c o n s i d e r a t i o n of n i t r o g e n r e c y c l i n g , a minimal annual p r o d u c t i o n of $40 g C yr-l a t a C/N r a t i o o f 5/1 gen s o u r c e . (Lee e t a l .

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