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Abundance and elemental composition of particulate matter in the upper layer of northeastern mediterranean

机译:东北地中海上层颗粒物的丰度和元素组成

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摘要

Suspended particulate (POC, PON, PP) profiles obtained in 1991-1994 indicate the existence of characteristic subsurface maxima near the base of the euphotic zone in the cyclonic Rhodes gyre and its peripherial waters in the Northeastern Mediterranean. Interestingly the N:P of the bulk seston was reasonable during stratification seasons when the surface water was relatively poor in phosphate; but the ratio was unexpectedly low (N:P=6-12) in the late winter of 1992 when the surface layer of Rhodes gyre was occupied with nutrient rich deep waters.
机译:1991-1994年获得的悬浮颗粒(POC,PON,PP)剖面表明,在东北地中海的旋风罗得岛回旋区及其外围水域中,在富营养区底部附近存在着特征性的地下最大值。有趣的是,在分层季节,当地表水的磷酸盐含量相对较低时,大体积石棉的N:P是合理的。但是在1992年冬末,当罗得斯回旋的表层被营养丰富的深水所占据时,该比率出乎意料地低(N:P = 6-12)。

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