2001
DOI: 10.1007/978-3-662-04482-7_12
|View full text |Cite
|
Sign up to set email alerts
|

The Convergence Ecosystem in the Southwest Atlantic

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
33
0

Year Published

2003
2003
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 48 publications
(33 citation statements)
references
References 20 publications
0
33
0
Order By: Relevance
“…Importantly, the highest reproductive intensity of X. kroyeri observed in this study not only occurred when temperature was high but also at a time of the year (spring and summer) when the SACW intrudes into the continental shelf (Pires 1992). This water mass transports nutrients to the studied region due to its high nitrogen to phosphorus ratio (N:P = 16:1) that favors primary productivity (Aidar et al 1993, Odebrecht & Castello 2001. Food availability for larvae (e.g.…”
mentioning
confidence: 76%
See 1 more Smart Citation
“…Importantly, the highest reproductive intensity of X. kroyeri observed in this study not only occurred when temperature was high but also at a time of the year (spring and summer) when the SACW intrudes into the continental shelf (Pires 1992). This water mass transports nutrients to the studied region due to its high nitrogen to phosphorus ratio (N:P = 16:1) that favors primary productivity (Aidar et al 1993, Odebrecht & Castello 2001. Food availability for larvae (e.g.…”
mentioning
confidence: 76%
“…Exchange of water and sediment between the coastal region and the adjacent shelf is very limited 58 Almeida et al: MPA benefits to overfished shrimp populations (Mahiques 1995). This region is affected by 3 water masses: coastal water (CW: temperature > 20°C, salinity < 36 PSU), tropical water (TW: > 20°C, > 36 PSU) and South Atlantic central water (SACW: <18°C, < 36 PSU) (Castro-Filho et al 1987, Odebrecht & Castello 2001. During summer, the SACW penetrates into the bottom layer of the coastal region and forms a thermocline over the inner shelf located at depths of 10 to 15 m. During winter, the SACW retreats to the shelf break and is replaced by the CW.…”
mentioning
confidence: 99%
“…The confluence of tropical waters from the Brazil Current with subantarctic waters from the Falklands Current occurs between latitudes 30º and 46º S. This subtropical convergence in the southwestern Atlantic (Pires 1992) forms a water mass called the South Atlantic Central Water (SACW). During certain times of the year, this water mass, depending on the intensity and influence of currents and winds (Castro-Filho et al 1987), can influence coastal regions, causing horizontal and vertical changes, as well as seasonal mixing of tropical and subantarctic waters (Odebrecht and Castello 2001). Changes in bottom and surface temperatures and salinity are related to the hydrodynamics of the water masses in the Ubatuba region (see Pires 1992).…”
Section: Discussionmentioning
confidence: 99%
“…This probably results from the higher plankton productivity during the summer in Ubatuba, when the South Atlantic Central Water (SACW) penetrates the bottom layer over the continental shelf and reaches the coast (Pires-Vanin & Matsuura 1993). The SACW is a nutrient-rich water mass with an N:P ratio (nitrogen: phosphorus) of approximately 16:1, favoring primary productivity (Odebrecht & Castello 2001). According to Vega-Perez (1993), the presence of this water mass in Ubatuba is responsible, among other factors, for the increase in chlorophyll content, and consequently the increase in phytoplankton growth.…”
Section: Discussionmentioning
confidence: 99%