The occurrence of total P (P-TOT) and the mineral forms of P (P-MIN) [
P bonded with Ca (P-Ca), Fe (P-Fe) and Al (P-Al)] in sediments from th
e Gulf of Gdarisk were investigated. Significant variations in the for
ms of P with depth in the sediment column were observed. P-Ca is the d
ominant form in the sediments except in the surface sediments of the d
eep areas of the Gulf of Gdansk where organic P (P-ORG) is dominant. T
hese areas also contain the highest contents of P-TOT in the region. (
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